事件沉积学——发展历程、研究现状及未来趋势

田景春 ,  张翔 ,  林小兵 ,  梁庆韶 ,  王峰 ,  孟万斌 ,  杨田

成都理工大学学报(自然科学版) ›› 2026, Vol. 53 ›› Issue (4) : 891 -914.

PDF (6281KB)
成都理工大学学报(自然科学版) ›› 2026, Vol. 53 ›› Issue (4) : 891 -914. DOI: 10.12474/cdlgzrkx.2026042101
成都理工大学70周年校庆专刊

事件沉积学——发展历程、研究现状及未来趋势

作者信息 +

Event sedimentology: development history, research progress, and future perspectives

Author information +
文章历史 +
PDF (6431K)

摘要

事件沉积学作为沉积学的重要分支学科之一,专注于研究地质历史时期各类突发性地质事件(如地震、洪水、风暴、浊流、火山喷发等)所形成的事件沉积层的特征、成因机制与分布规律,为深刻认识沉积圈层演化、重建地球演化史提供关键证据。本文在系统梳理事件沉积学领域前人研究成果的基础上,全面阐述了事件沉积学的发展历程,主要包括:思想萌芽、理论奠基、学科形成和快速发展4个阶段;系统总结了中外对地震、洪水、冰川、风暴、海啸、碎屑流、浊流、缺氧及火山等9类事件沉积研究所取得的进展,分析了中外研究成果的异同,明确了下一步研究的重点,包括建立多指标判识标志、定量反演事件发生的周期及强度、厘定多事件耦合关系、阐明事件沉积的环境、资源意义等。深入探讨了事件沉积学未来深化发展的4个主要方向,包括:向高精度、多指标、定量化表征方向迈进;强化多类型事件沉积的耦合与“事件链”系统研究;深化多学科交叉融合,催生新的理论生长点;拓展学科应用领域,服务国家重大战略。总之,事件沉积学通过解码沉积圈中的“事件记忆”层,有助于深化对地史时期与现代突发性地质事件的认知,其发展必将成为预测未来地球系统行为、保障资源安全与防范灾害风险的关键基础学科之一。

Abstract

Event sedimentology, as one of the most important branches of sedimentology, focuses on the characteristics, genetic mechanisms, and distribution patterns of event deposits formed by various episodic geological events throughout Earth’s history, such as earthquakes, floods, storms, turbidity currents, and volcanic eruptions. It provides critical evidence for understanding the evolution of sedimentary systems and reconstructing Earth's evolutionary history. Based on a comprehensive review of previous studies in the field, this paper systematically outlines the developmental history of event sedimentology, which can be divided into four major stages: conceptual emergence, theoretical foundation, disciplinary establishment, and rapid development. Furthermore, the research progress on nine major types of event deposits, including seismic, flood, glacial, storm, tsunami, debris-flow, turbidite, anoxic, and volcanic deposits, is comprehensively summarized. Similarities and differences between domestic and international studies are analyzed, and key future research priorities are identified, including the establishment of multi-proxy identification criteria, quantitative reconstruction of event periodicity and intensity, clarification of the coupling relationships among multiple events, and elucidation of the environmental and resource significance of event deposits. The paper also discusses four major directions for the future advancement of event sedimentology: (1) developing toward high-resolution, multi-proxy, and quantitative characterization; (2) strengthening research on the coupling of multiple event deposits and integrated “event-chain” systems; (3) promoting interdisciplinary integration to foster new theoretical breakthroughs; and (4) expanding application fields to support major national strategic needs. In summary, by decoding the “event memory” preserved within sedimentary records, event sedimentology enhances our understanding of both ancient and modern episodic geological events. Its continued development will undoubtedly establish it as a key foundational discipline for predicting future Earth system behavior, ensuring resource security, and mitigating geological hazards.

关键词

事件沉积学 / 发展历史 / 研究现状 / 发展趋势 / 综述

Key words

event sedimentology / development history / research progress / development trends / review

引用本文

引用格式 ▾
田景春,张翔,林小兵,梁庆韶,王峰,孟万斌,杨田. 事件沉积学——发展历程、研究现状及未来趋势[J]. 成都理工大学学报(自然科学版), 2026, 53(4): 891-914 DOI:10.12474/cdlgzrkx.2026042101

登录浏览全文

4963

注册一个新账户 忘记密码

参考文献

[1]

柴之芳, 马淑兰, 毛雪瑛, 等, 1986. 浙江长兴二叠系/三叠系界线剖面的元素地球化学特征[J]. 地质学报,(2): 139-150.

[2]

Chai Z F, Ma S L, Mao X Y, et al., 1986. Elemental geochemical characters at the Permian-Triassic boundary section in Changxing, Zhejiang, China[J]. Acta Geological Sinica, (2): 139-150. (in Chinese)

[3]

陈兰, 达雪娟, 朱章雄, 等, 2025. 托阿尔期大洋缺氧事件在中国陆相地层的碳循环扰动响应[J]. 古地理学报, 27(2): 528-540.

[4]

Chen L, Da X J, Zhu Z X, et al., 2025. Response to carbon cycle perturbation during the Toarcian oceanic anoxic event in terrestrial strata of China[J]. Journal of Palaeogeography (Chinese Edition), 27(2): 528-540. (in Chinese)

[5]

成乐乐, 金思丁, 韩中, 等, 2024. 早侏罗世托阿尔期大洋缺氧事件的天文年代学对比研究[J]. 第四纪研究, 44(5): 1141-1162.

[6]

Cheng L L, Jin S D, Han Z, et al., 2024. Astrochronological comparative study of the Early Jurassic Toarcian oceanic anoxic event[J]. Quaternary Sciences, 44(5): 1141-1162. (in Chinese)

[7]

冯先岳, 1989. 地震振动液化形变的研究[J]. 内陆地震,(4): 299-307.

[8]

Feng X Y, 1989. Study on the deformation caused by seismic vibrational liquefaction[J]. Inland Earthquake, (4): 299-307. (in Chinese)

[9]

付金华, 罗顺社, 牛小兵, 等, 2015. 鄂尔多斯盆地陇东地区长7段沟道型重力流沉积特征研究[J]. 矿物岩石地球化学通报, 34(1): 29-37.

[10]

Fu J H, Luo S S, Niu X B, et al., 2015. Sedimentary characteris-tics of channel type gravity flow of the member 7 of Yanchang Formation in the Longdong area,Ordos Basin[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 34(1): 29-37. (in Chinese)

[11]

傅强, 李璟, 邓秀琴, 等, 2019. 沉积事件对深水沉积过程的影响——以鄂尔多斯盆地华庆地区长6油层组为例[J]. 岩性油气藏, 31(1): 20-29.

[12]

Fu Q, Li J, Deng X Q, et al., 2019. Influence of sedimentary events on deep water sedimentation process:a case of Chang 6 reservoir in Huaqing area, Ordos Basin[J]. Lithologic Reservoirs, 31(1): 20-29. (in Chinese)

[13]

傅强, 吕苗苗, 刘永斗, 2008. 鄂尔多斯盆地晚三叠世湖盆浊积岩发育特征及地质意义[J]. 沉积学报, 26(2): 186-192.

[14]

Fu Q, Lü M M, Liu Y D, 2008. Developmental characteristics of turbidite and its implication on petroleum geology in Late-Triassic Ordos Basin[J]. Acta Sedimentologica Sinica, 26(2): 186-192. (in Chinese)

[15]

郭召杰, 朱贝, 陈石, 2015. 熔积岩及其对中国几处关键构造事件的限定[J]. 地学前缘, 22(2): 174-186.

[16]

Guo Z J, Zhu B, Chen S, 2015. Peperite:constraints to a few key tectonic events in China[J]. Earth Science Frontiers, 22(2): 174-186. (in Chinese)

[17]

韩作振, 宋志刚, 高丽华, 等, 2017. 吉林省“大黑山条垒带”晚古生代火山事件及其构造意义[J]. 地学前缘, 24(2): 186-201.

[18]

Han Z Z, Song Z G, Gao L H, et al., 2017. Late Paleozoic volcanic events in “ Daheishan Horst” in Jilin, China and their tectonic significance[J]. Earth Science Frontiers, 24(2): 186-201. (in Chinese)

[19]

何起祥, 2003. 沉积地球科学的历史回顾与展望[J]. 沉积学报,(1): 10-18.

[20]

He Q X, 2003. Sedimentary earth sciences:yesterday,today and tomorrow[J]. Acta Sedimentologica Sinica,(1): 10-18.(in Chinese)

[21]

侯方浩, 方少仙, 董兆雄, 等, 2003. 鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征[J]. 沉积学报, 21(1): 106-112.

[22]

Hou F H, Fang S X, Dong Z X, et al., 2003. The developmental characters of sedimentary environments and lithofacies of Middle Ordovician Majiagou Formation in Ordos Basin[J]. Acta Sedimentologica Sinica, 21(1): 106-112. (in Chinese)

[23]

胡明毅, 贺萍, 2002. 潮坪风暴沉积特征及其研究意义[J]. 地球科学进展, 17(3): 391-395.

[24]

Hu M Y, He P, 2002. The study of tidal storm deposits and its research signifciance[J]. Advances in Earth Science, 17(3): 391-395. (in Chinese)

[25]

黄道全, 1988. 冰成岩分类命名的探讨[J]. 岩石学报, 4(3): 54-62.

[26]

Huang D Q, 1988. On the classification and nomenclature of glacious rocks[J]. Acta Petrologica Sinica, 4(3): 54-62. (in Chinese)

[27]

姜在兴, 赵徵林, 刘孟慧, 1988. 一种沿深水箕状谷纵向搬运的重力流沉积[J]. 石油实验地质, 10(2): 106-116.

[28]

Jiang Z X, Zhao Z L, Liu M H, 1988. Replaced deposition of grav-ity flows along moving a deep water dustpan thalweg[J]. Petroleum Geology & Experiment, 10(2): 106-116. (in Chinese)

[29]

姜在兴, 赵澂林, 刘孟慧, 等, 1990. 东濮凹陷西部湖相风暴沉积的初步研究[J]. 沉积学报, 8(1): 107-114.

[30]

Jiang Z X, Zhao C L, Liu M H, et al., 1990. Preliminary research into lacustrine storm-current deposits:an example from the western Dongpu depression[J]. Acta Sedimentologica Sinica, 8(1): 107-114. (in Chinese)

[31]

李继亮, 陈昌明, 高文学, 等, 1978. 我国几个地区浊积岩系的特征[J]. 地质科学, 13(1): 26-44.

[32]

Li J L, Chen C M, Gao W X, et al., 1978. On the features of turbidite sequences in some regions of China[J]. Chinese Journal of Geology, 13(1): 26-44. (in Chinese)

[33]

李四光, 赵亚曾, 1924. 长江峡东地质及峡之历史[J]. 中国地质学会志, 3(3/4): 351-392.

[34]

李相博, 卫平生, 刘化清, 等, 2013. 浅谈沉积物重力流分类与深水沉积模式[J]. 地质论评, 59(4): 607-614.

[35]

Li X B, Wei P S, Liu H Q, et al., 2013. Discussion on the classifi-cation of sediment gravity flow and the deep-water sedimen-tary model[J]. Geological Review, 59(4): 607-614. (in Chinese)

[36]

刘宝珺, 张继庆, 许效松, 1986. 四川兴文四龙下二叠统碳酸盐风暴岩[J]. 地质学报, 60(1): 55-67.

[37]

Liu B J, Zhang J Q, Xu X S, 1986. On the calcareous tempestites in the Lower Permian of Silong,Xingwen,Sichuan[J]. Acta Geologica Sinica, 60(1): 55-67. (in Chinese)

[38]

刘忠宝, 于炳松, 陈晓林, 等, 2003. 塔里木盆地塔东地区中-上奥陶统海底扇浊积岩层序地层格架及沉积特征[J]. 现代地质, 17(4): 408-414.

[39]

Liu Z B, Yu B S, Chen X L, et al., 2003. Sequence stratigraphy and sedimentary characters of submarine fan of Middle-Upper Ordovician in Tadong area, the Tarim Basin[J]. Geoscience, 17(4): 408-414. (in Chinese)

[40]

吕奇奇, 罗顺社, 李梦杰, 等, 2020. 深水碎屑流与浊流混合事件层沉积特征及分布——以鄂尔多斯盆地西南长7油层组为例[J]. 东北石油大学学报, 44(2): 69-78.

[41]

Lü Q Q, Luo S S, Li M J, et al., 2020. Sedimentary characteristics and distribution of deep-water hybrid event beds comprising debris and turbidites:a case study of Chang7 oil formation in the southwest of Ordos Basin[J]. Journal of Northeast Petroleum University, 44(2): 69-78. (in Chinese)

[42]

吕奇奇, 王林, 罗顺社, 等, 2025. 湖相细粒浊流沉积动力学机制初探——基于水槽沉积模拟实验[J]. 沉积学报, 43(3): 769-781.

[43]

Lü Q Q, Wang L, Luo S S, et al., 2025. Preliminary study of the dynamic mechanism of lacustrine fine-grained turbidity deposits based on a flume sedimentary simulation[J]. Acta Sedimentologica Sinica, 43(3): 769-781. (in Chinese)

[44]

马俊学, 2017. 岷江上游叠溪古堰塞湖溃坝堆积体的沉积特征及溃决洪水反演[D]. 北京:中国地质大学(北京).

[45]

Ma J X, 2017. Sedimentary characteristics of outburst deposits and inversion of outburst flood induced by the Diexi paleo dammed lake of the Upper Minjiang River in China[D]. Beijing: China University of Geosciences (Beijing). (in Chinese)

[46]

潘树新, 郑荣才, 卫平生, 等, 2013. 陆相湖盆块体搬运体的沉积特征、识别标志与形成机制[J]. 岩性油气藏, 25(2): 9-18.

[47]

Pan S X, Zheng R C, Wei P S, et al., 2013. Deposition characteris-tics,recognition mark and form mechanism of mass trans-port deposits in terrestrial lake Basin[J]. Lithologic Reser-voirs, 25(2): 9-18. (in Chinese)

[48]

乔秀夫, 李海兵, 2009. 沉积物的地震及古地震效应[J]. 古地理学报, 11(6): 593-610.

[49]

Qiao X F, Li H B, 2009. Effect of earthquake and ancient earth-quake on sediments[J]. Journal of Palaeogeography, 11(6): 593-610. (in Chinese)

[50]

宋天锐, 1988. 北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震−海啸序列[J]. 科学通报, 33(8): 609-611.

[51]

Song T R, 1988. A probable earthquake-tsunami sequence in Precambrian carbonate strata of Ming Tombs district, Beijing[J]. Chinese Science Bulletin, 33(13):1121-1124.

[52]

孙宁亮, 钟建华, 田东恩, 等, 2017. 鄂尔多斯盆地南部延长组事件沉积与致密油的关系[J]. 中国石油大学学报(自然科学版), 41(6): 30-40.

[53]

Sun N L, Zhong J H, Tian D E, et al., 2017. Relationship between event deposits and tight oil of Yanchang Formation in south-ern Ordos Basin[J]. Journal of China University of Petroleum (Edition of Natural Science), 41(6): 30-40. (in Chinese)

[54]

田景春, 2014. 事件沉积学[M]. 北京:地质出版社.

[55]

Tian J C, 2014. Event sedimentology[M]. Beijing: Geological Publishing House. (in Chinese)

[56]

田景春, 梁庆韶, 王峰, 等, 2022. 陆相湖盆致密油储集砂体成因及发育模式——以鄂尔多斯盆地上三叠统长6油层组为例[J]. 石油与天然气地质, 43(4): 877-888.

[57]

Tian J C, Liang Q S, Wang F, et al., 2022. Genetic origin and development model of tight oil reservoir sand bodies in continental lacustrine basins:a case study of the Chang 6 oil layer group of the Upper Triassic, Ordos Basin[J]. Oil and Gas Geology, 43(4): 877-888. (in Chinese)

[58]

田景春, 梁庆韶, 王峰, 等, 2026. 鄂尔多斯盆地延长组事件沉积学研究[M]. 北京:科学出版社.

[59]

Tian J C, Liang Q S, Wang F, et al., 2026. Study of event sedi-mentology of the Yanchang Formation in the Ordos Basin[M]. Beijing:Science Press. (in Chinese)

[60]

田景春, 文华国, 张翔, 等, 2024. 沉积地质学研究生系列教材持续建设探索——以成都理工大学为例[J]. 成都理工大学学报(社会科学版), 32(6): 103-112.

[61]

Tian J C, Wen H G, Zhang X, et al., 2024. Exploration of continu-ous construction of graduate textbook series in sedimentary geology: a case study of Chengdu University of Technology[J]. Journal of Chengdu University of Technol-ogy (Social Sciences), 32(6): 103-112. (in Chinese)

[62]

王成善, 马永生, 彭平安, 等, 2025. 从沉积学到沉积圈科学:百年简要回顾与发展展望[J]. 沉积学报, 43(5): 1535-1554.

[63]

Wang C S, Ma Y S, Peng P A, et al., 2025. A century journey from sedimentology to sedimentosphere science:review and perspective[J]. Acta Sedimentologica Sinica, 43(5): 1535-1554. (in Chinese)

[64]

王伟涛, 杨小强, 舒鹏, 等, 2025. 华南沿海珠江口约 1 000 a前海啸事件的沉积记录与海啸源分析[J]. 地震地质, 47(4): 999-1019.

[65]

Wang W T, Yang X Q, Shu P, et al., 2025. Sedimentary records and source analysis of a tsunami event about ~1 000 years ago in the Pearl River estuary along the coast of South China[J]. Seismology and Geology, 47(4): 999-1019. (in Chinese)

[66]

王小妮, 杨智, 冯有良, 等, 2024. 咸水湖泊细粒重力流沉积及油气意义:以柴达木盆地英西地区下干柴沟组上段为例[J]. 古地理学报, 26(4): 985-1004.

[67]

Wang X N, Yang Z, Feng Y L, et al., 2024. Fine-grained gravity flow deposits and their petroleum significance in saline lacustrine basins:a case study from the upper member of Lower Ganchaigou Formation in Yingxi area of Qaidam Basin, China[J]. Journal of Palaeogeography (Chinese Edition), 26(4): 985-1004. (in Chinese)

[68]

王喻鸣, 王玉琨, 李琳琳, 等, 2023. 南海北部海域北宋年间的古海啸记录及其潜在触发机制[J]. 科学通报, 68(20): 2690-2708.

[69]

Wang Y M, Wang Y K, Li L L, et al., 2023. Paleo-tsunami sedi-mentary records and potential triggering mechanism during the Earlier Song Dynasty at the northern South China Sea[J]. Chinese Science Bulletin, 68(20): 2690-2708. (in Chinese)

[70]

魏魁生, 叶淑芬, 郭占谦, 等, 1996. 松辽盆地白垩系非海相沉积层序模式[J]. 沉积学报, 14(4): 50-60.

[71]

Wei K S, Ye S F, Guo Z Q, et al., 1996. Sequence stratigraphic model of nonmarine sediments in Cretaceous, Songliao Basin[J]. Acta Sedimentologica Sinica, 14(4): 50-60. (in Chinese)

[72]

吴崇筠, 1986. 湖盆砂体类型[J]. 沉积学报, 4(4): 1-27.

[73]

Wu C Y, 1986. Sandbodies in lake basin[J]. Acta Sedimentolog-ica Sinica, 4(4): 1-27. (in Chinese)

[74]

吴瑞棠, 杨玉卿, 1991. 冰川事件的识别标志[J]. 地球科学——中国地质大学学报, 16(4): 353-359.

[75]

Wu R T, Yang Y Q, 1991. The indicators for recognizing glacial event[J]. Earth Science-Journal of China University of Geosciences, 16(4): 353-359. (in Chinese)

[76]

吴贤涛, 尹国勋, 1992. 四川峨眉晚侏罗世湖泊沉积中震积岩的发现及其意义[J]. 沉积学报, 10(1): 19-26.

[77]

Wu X T, Yi G X, 1992. Features and significance of seismites from upper Jurasic lacustrine deposites of Emei,Sichuan[J]. Acta Sedimentologica Sinica, 10(1): 19-26. (in Chinese)

[78]

夏青松, 田景春, 黄昌武, 2007. 鄂尔多斯盆地上三叠统延长组震积岩识别标志研究[J]. 成都理工大学学报(自然科学版), 34(3): 312-317.

[79]

Xia Q S, Tian J C, Huang C W, 2007. Study on the recognition marks of seismites in Upper Triassic Yanchang Formation, Ordos Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 34(3): 312-317. (in Chinese)

[80]

徐道一, 卢演俦, 1985. 陆相和海相地层的天文对比方法[J]. 地层学杂志, 9(3): 195-202.

[81]

许靖华, 奥伯亨斯利 H., 高计元, 等, 1986. 寒武纪生物爆发前的死劫难海洋[J]. 地质科学, 21( 1): 1-6.

[82]

Xu J H, Oberhänsli H, Gao J Y, et al., 1986. Strangelove ocean before the Cambrian explosion[J]. Chinese Journal of Geol-ogy, 21( 1): 1-6. (in Chinese)

[83]

鄢继华, 陈世悦, 姜在兴, 等, 2007. 断陷湖盆震浊积岩成因模拟实验[J]. 古地理学报, 9(3): 277-282.

[84]

Yan J H, Chen S Y, Jiang Z X, et al., 2007. Simulating experi-ment on genesis of seismo-turbidites in rift lacustrine basin[J]. Journal of Palaeogeography, 9(3): 277-282. (in Chinese)

[85]

严兆彬, 郭福生, 彭花明, 等, 2014. 浙西下寒武统大陈岭组沉积异常及其海啸成因初探[J]. 沉积学报, 32(3): 459-467.

[86]

Yan Z B, Guo F S, Peng H M, et al., 2014. Preliminary study on abnormal sediments and their tsunami origin of the Lower Cambrian the Dachenling Formation in western Zhejiang[J]. Acta Sedimentologica Sinica, 32(3): 459-467. (in Chinese)

[87]

杨华, 牛小兵, 罗顺社, 等, 2015. 鄂尔多斯盆地陇东地区长7段致密砂体重力流沉积模拟实验研究[J]. 地学前缘, 22(3): 322-332.

[88]

Yang H, Niu X B, Luo S S, et al., 2015. Research of simulated experiment on gravity flow deposits of tight sand bodies of Chang 7 Formation in Longdong area,Ordos Basin[J]. Earth Science Frontiers, 22(3): 322-332. (in Chinese)

[89]

杨剑萍, 王辉, 陈世悦, 等, 2004. 济阳坳陷古近系震积岩特征[J]. 沉积学报, 22(2): 281-287.

[90]

Yang J P, Wang H, Chen S Y, et al., 2004. The features of seis-mite in Jiyang sub-basin,Paleogene[J]. Acta Sedimentolog-ica Sinica, 22(2): 281-287. (in Chinese)

[91]

杨劲松, 王永, 尹金辉, 等, 2022. 我国冲积平原区洪水事件重建研究进展及展望[J]. 地球科学, 47(11): 3944-3959.

[92]

Yang J S, Wang Y, Yin J H, et al., 2022. Progress and prospects in reconstruction of flood events in Chinese alluvial plains[J]. Earth Science, 47(11): 3944-3959. (in Chinese)

[93]

杨仁超, 何治亮, 邱桂强, 等, 2014. 鄂尔多斯盆地南部晚三叠世重力流沉积体系[J]. 石油勘探与开发, 41(6): 661-670.

[94]

Yang R C, He Z L, Qiu G Q, et al., 2014. Late Triassic gravity flow depositional systems in the southern Ordos Basin[J]. Petroleum Exploration and Development, 41(6): 661-670. (in Chinese)

[95]

杨仁超, 李作福, 张学才, 等, 2023. 异重流沉积研究进展与展望[J]. 沉积学报, 41(6): 1917-1933.

[96]

Yang R C, Li Z F, Zhang X C, et al., 2023. Advances and perspec-tives in the study of hyperpycnal flow deposition[J]. Acta Sedimentologica Sinica, 41(6): 1917-1933. (in Chinese)

[97]

杨田, 操应长, 田景春, 等, 2025. 沉积物重力流搬运演化与沉积过程[J]. 沉积学报, 43(5): 1625-1641.

[98]

Yang T, Cao Y C, Tian J C, et al., 2025. Transport,evolution and depositional processes of sediment gravity flows[J]. Acta Sedimentologica Sinica, 43(5): 1625-1641. (in Chinese)

[99]

余斌, 章书成, 王士革, 2005. 四川西昌邛海的浊流沉积初探[J]. 沉积学报, 23(4): 559-565.

[100]

Yu B, Zhang S C, Wang S G, 2005. A preliminary study on the deposition of turbidity currents in Qionghai Lake,Sichuan, China[J]. Acta Sedimentologica Sinica, 23(4): 559-565. (in Chinese)

[101]

苑书金, 李发有, 陆文明, 2025. 加密井快速优化技术在西非深水浊积砂油藏精细描述中的应用——以 Bata 油田为例[J]. 物探与化探, 49(6): 1303-1310.

[102]

Yuan S J, Li F Y, Lu W M, 2025. Application of rapid infill-well optimization technology in fine-scale description of deep-water turbidite reservoirs in West Africa:a case study of the Bata oilfield[J]. Geophysical and Geochemical Exploration, 49(6): 1303-1310. (in Chinese)

[103]

袁珍, 李文厚, 杨喜彦, 等, 2019. 鄂尔多斯盆地三叠系延长组事件沉积及其地质意义[J]. 西北大学学报(自然科学版), 49(3): 406-416.

[104]

Yuan Z, Li W H, Yang X Y, et al., 2019. Research on event deposits and its geologic significance of Yanchang Forma-tion in Ordos Basin[J]. Journal of Northwest University (Natural Science Edition), 49(3): 406-416. (in Chinese)

[105]

曾建理, 张廷山,

[106]

Popa M E, 等, 2024. 三叠纪末期四川盆地湖泊风暴记录及其驱动机制[J]. 中国科学:地球科学, 54(7): 2419-2436. Zeng J L, Zhang T S, Popa M E, et al., 2024. End-Triassic storm deposits in the lacustrine Sichuan Basin and their driving mechanisms[J]. Science China Earth Sciences, 67(7):2383-2400.

[107]

曾雄伟, 周鹏, 刘安, 等, 2014. 三峡东部地区泥盆系写经寺组下部一套可能的海啸沉积[J]. 沉积学报, 32(5): 816-822.

[108]

Zeng X W, Zhou P, Liu A, et al., 2014. A possible tsunami deposits in the lower part of the Devonian Xiejingsi Forma-tion in the East Yangtze Gorges area[J]. Acta Sedimentolog-ica Sinica, 32(5): 816-822. (in Chinese)

[109]

章诚诚, 方朝刚, 刘桃, 等, 2024. 沉积盆地洪水异重流研究进展[J]. 华东地质, 45(1): 49-61.

[110]

Zhang C C, Fang C G, Liu T, et al., 2024. Research progress on flood-triggered hyperpycnal flows in sedimentary basins[J]. East China Geology, 45(1): 49-61. (in Chinese)

[111]

张继庆, 冯纯江, 杜德勋, 1986. 四川下二叠统风暴岩的发现及风暴沉积作用的研究[C]//中国地质学会海洋地质专业委员会. 中国地质学会海洋地质专业委员会硫酸盐比较沉积学学术讨论会,成都:地矿部成都地质矿产研究所: 15.

[112]

Zhang J Q, Feng C J, Du D X, 1986. Discovery of tempestites in the Lower Permian of Sichuan and study of storm sedimenta-tion[C]//Marine Geology Committee of the Geological Soci-ety of China. Symposium on Comparative Sedimentology of Sulfates,Marine Geology Professional Committee,Geologi-cal Society of China,Chengdu:Chengdu Institute of Geol-ogy and Mineral Resources, Ministry of Geology and Mineral Resources: 15. (in Chinese)

[113]

张勤文, 徐道一, 杨正宗, 等, 1984. 类地天体与地球地质作用的比较研究[J]. 中国地质科学院院报,(2): 237-246.

[114]

Zhang Q W, Xu D Y, Yang Z Z, et al., 1984. The comparison of geological processes of the Earth with the Earth-like celes-tial bodies[J]. Bulletin of the Chinese Academy of Geologi-cal Sciences,(2): 237-246. (in Chinese)

[115]

张廷山, 杜翔, 杨巍, 等, 2017. 米仓山前缘早志留世软沉积物变形构造及其触发机制[J]. 沉积学报, 35(2): 253-263.

[116]

Zhang T S, Du X, Yang W, et al., 2017. A discussion on deforma-tion structures of early Silurian soft sediment and its trigger mechanism in the front of Micangshan Mountain[J]. Acta Sedimentologica Sinica, 35(2): 253-263. (in Chinese)

[117]

赵梅, 2012. 渭河中游古洪水滞流沉积物特征研究[D]. 西安: 陕西师范大学.

[118]

周炼, 苏洁, 黄俊华, 等, 2011. 判识缺氧事件的地球化学新标志——钼同位素[J]. 中国科学:地球科学, 41(3): 309-319.

[119]

Zhou L, Su J, Huang J H, et al., 2011. A new paleoenvironmental index for anoxic events-Mo isotopes in black shales from Upper Yangtze marine sediments[J]. Science China Earth Sciences,54(7):1024-1033.

[120]

朱日祥, 王华建, 张旺, 等, 2026. 白垩系全球油气富集的多圈层驱动机制[J/OL]. 地学前缘, 2026-02-13. https://doi.org/10.13745/j.esf.sf.2026.1.15.

[121]

Zhu R X, Wang H J, Zhang W, et al., 2026. Multi-spheric interac-tions driven global enrichment of Cretaceous hydrocarbons [J/OL]. Earth Science Frontiers, 2026-02-13. https://doi.org/10.13745/j.esf.sf.2026.1.15. (in Chinese)

[122]

邹才能, 赵政璋, 杨华, 等, 2009. 陆相湖盆深水砂质碎屑流成因机制与分布特征——以鄂尔多斯盆地为例[J]. 沉积学报, 27(6): 1065-1075.

[123]

Zou C N, Zhao Z Z, Yang H, et al., 2009. Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J]. Acta Sedimentologica Sinica, 27(6): 1065-1075. (in Chinese)

[124]

Agassiz L, 1838. Upon glaciers, moraines, and erratic blocks[J]. The Edinburgh New Philosophical Journal, 24: 864-883.

[125]

Al-Saqarat B S, Abbas M, Al Hseinat M, et al., 2024. Interpreting soft-sediment deformation structures: insights into earth-quake history and depositional processes in the Dead Sea, Jordan[J]. Geosciences, 14(8): 217.

[126]

Aigner T, 1982. Calcareous tempestites:storm-dominated stratifi-cation in Upper Muschelkalk limestones (Middle Trias,SW-Germany)[C]// Einsele G, Seilacher A. Cyclic and Event Stratification. Berlin:Springer-Verlag: 180-198.

[127]

Aigner T, 1985. Storm depositional systems:dynamic stratigraphy in modern and ancient shallow-marine sequences[M]// Aigner T. Lecture notes in Earth sciences,Vol. 3,Berlin:Springer-Verlag.

[128]

Allen J R L, 1982. Sedimentary structures: their character and physical basis[M]. Amsterdam:Elsevier.

[129]

Alvarez L W, Alvarez W, Asaro F, et al., 1980. Extraterrestrial cause for the Cretaceous-Tertiary extinction[J]. Science, 208(4448): 1095-1108.

[130]

Baker V R, 1987. Paleoflood hydrology and extraordinary flood events[J]. Journal of Hydrology, 96(1/2/3/4): 79-99.

[131]

Baker V R, 2008. Paleoflood hydrology: origin, progress,prospects[J]. Geomorphology, 101(1/2): 1-13.

[132]

Batubo P, Morra G, Oppo D, et al., 2024. A medium-sized paleo-tsunami reconstruction by a deep neural network processing sedimentary deposits[J]. Earth and Space Science, 11(1): e2023EA003216.

[133]

Bauerman H, 1885. Report on the geology of the country near the forty-ninth parallel of north latitude, west of the Rocky Mountains[R]. Canada Geological Survey Report Program,1882-1884, Part B: 1-42.

[134]

Bernhardt A, Stright L, Lowe D R, 2012. Channelized debris-flow deposits and their impact on turbidity currents: the Puchkirchen axial channel belt in the Austrian Molasse Basin[J]. Sedimentology, 59(7): 2042-2070.

[135]

Bond D P G, Wignall P B, 2010. Pyrite framboid study of marine Permian-Triassic boundary sections:a complex anoxic event and its relationship to contemporaneous mass extinction[J]. Geological Society of America Bulletin, 122(7/8): 1265-1279.

[136]

Boulton G S, 1982. Subglacial processes and the development of glacial bedforms[J]. Research in glacial,glacio-fluvial,and glacio-lacustrine systems. Proc. 6th Guelph symposium on geomorphology,1980: 1-31.

[137]

Bouma A H, 1962. Sedimentology of some flysch deposits: a graphic approach to facies interpretation[M]. Amsterdam:Elsevier: 168.

[138]

Bourgeois J, Hansen T A, Wiberg P L, et al., 1988. A tsunami deposit at the Cretaceous-Tertiary boundary in Texas[J]. Science, 241(4865): 567-570.

[139]

Brenchley P J, Newall G, Stanistreet I G, 1979. A storm surge origin for sandstone beds in an epicontinental platform sequence, Ordovician, Norway[J]. Sedimentary Geology, 22(3/4): 185-217.

[140]

Chen X S, Kuang H W, Liu Y Q, et al., 2021. Revisiting the Nantuo Formation in Shennongjia,South China:a new depo-sitional model and multiple glacial cycles in the Cryogenian[J]. Precambrian Research, 356: 106132.

[141]

Chen X Y, Blockley S P E, Tarasov P E, et al., 2016. Clarifying the distal to proximal tephrochronology of the millennium (B-Tm) eruption,Changbaishan Volcano,northeast China[J]. Quaternary Geochronology, 33: 61-75.

[142]

Daly R A, 1936. Origin of submarine “ canyons” [J]. American Journal of Science, 31(186): 401-420.

[143]

Dawson A G, 1994. Geomorphological effects of tsunami run-up and backwash[C]// The 25th Binghamton Symposium in Geomorphology. Binghamton:Elsevier: 83-94.

[144]

Dawson A G, Stewart I, 2007. Tsunami deposits in the geological record[J]. Sedimentary Geology, 200(3/4): 166-183.

[145]

Demaison G J, Moore G T, 1980. Anoxic environments and oil source bed genesis[J]. Organic Geochemistry, 2(1): 9-31.

[146]

Dodd T J H, Leslie A G, Gillespie M R, et al., 2020. Deep to shal-low-marine sedimentology and impact of volcanism within the Middle Triassic Palaeo-Tethyan Semantan Basin,Singa-pore[J]. Journal of Asian Earth Sciences, 196: 104371.

[147]

Einsele G, 1996. Event deposits:the role of sediment supply and relative sea-level changes-overview[J]. Sedimentary Geol-ogy, 104(1/2/3/4): 11-37.

[148]

Einsele G, Seilacher A, 1982. Cyclic and event stratification[M]. Heidelberg: Springer-Verlag.

[149]

Forel F A, 1881. Ravins sous-lacustres des fleuves glaciaires[J]. Comptes Rendus de l’Académie des Sciences, 101(16): 725-728.

[150]

Fujino S, Masuda F, Tagomori S, et al., 2006. Structure and depo-sitional processes of a gravelly tsunami deposit in a shallow marine setting:Lower Cretaceous Miyako Group,Japan[J]. Sedimentary Geology, 187(3/4): 127-138.

[151]

Geikie A, 1863. On the phenomena of the glacial drift of Scotland[J]. Transactions of the Geological Society of Glas-gow, 1(2): 186-190.

[152]

Gilbert G K, 1899. Ripple-marks and cross-bedding[J]. Bulletin of the Geological Society of America, 10(1): 135-140.

[153]

Goff J, Pearce S, Nichol S L, et al., 2010. Multi-proxy records of regionally-sourced tsunamis,New Zealand[J]. Geomorphol-ogy, 118(3/4): 369-382.

[154]

Goff J, Chagué-Goff C, Nichol S, et al., 2012. Progress in palaeot-sunami research[J]. Sedimentary Geology, 243/244: 70-88.

[155]

Goldberg T, Poulton S W, Wagner T, et al., 2016. Molybdenum drawdown during Cretaceous Oceanic Anoxic Event 2[J]. Earth and Planetary Science Letters, 440: 81-91.

[156]

Hampton M A, 1972. The role of subaqueous debris flow in gener-ating turbidity currents[J]. Journal of Sedimentary Research, 42(4): 775-793.

[157]

Hatch F H, Rastall R H, 1913. The Petrology of the Sedimentary Rocks[M]. London:George Allen & Unwin Ltd.

[158]

Heim A, 1932. Bergsturz und menschenleben[M]. Zürich:Fretz & Wasmuth.

[159]

Hsü K J, 1983. Actualistic catastrophism:address of the retiring president of the international association of sedimentolo-gists[J]. Sedimentology, 30(1): 3-9.

[160]

Hussain A, Haughton P D W, Shannon P M, et al., 2020. High-resolution X-ray fluorescence profiling of hybrid event beds:implications for sediment gravity flow behaviour and deposit structure[J]. Sedimentology, 67(6): 2850-2882.

[161]

Jackson K, Rogers J A, Wang P, et al., 2024. Archaeo-tempestites and coastal taphonomy of shell-bearing sites:native Ameri-can sites in Florida as a case study[J]. Journal of Archaeolog-ical Method and Theory, 31(4): 1622-1667.

[162]

Jones C E, Halliday A N, Rea D K, et al., 1994. Neodymium isotopic variations in North Pacific modern silicate sediment and the insignificance of detrital REE contributions to seawater[J]. Earth and Planetary Science Letters, 127(1/2/3/4): 55-66.

[163]

Kataoka K S, Nagahashi Y, McArthur A, 2019. From sink to volcanic source: unravelling missing terrestrial eruption records by characterization and high-resolution chronology of lacustrine volcanic density flow deposits, Lake Inawashiro-ko,Fukushima,Japan[J]. Sedimentology, 66(7): 2784-2827.

[164]

Kelling G, Mullin P R, 1975. Graded limestones and limestone-quartzite couplets:possible storm-deposits from the Moroc-can Carboniferous[J]. Sedimentary Geology, 13(3): 161-190.

[165]

Kettler C, Phillips E, Pichler K, et al., 2023. 3D macro- and micro-fabric analyses of Neoproterozoic diamictites from the Valjean Hills, California (United States)[J]. Frontiers in Earth Science, 11: 929011.

[166]

Key R M, Liyungu A K, Njamu F M, et al., 2001. The western arm of the Lufilian Arc in NW Zambia and its potential for copper mineralization[J]. Journal of African Earth Sciences, 33(3/4): 503-528.

[167]

Kneller B, Buckee C, 2000. The structure and fluid mechanics of turbidity currents:a review of some recent studies and their geological implications[J]. Sedimentology, 47(S1): 62-94.

[168]

Kochel R C, Baker V R, 1982. Paleoflood hydrology[J]. Science, 215(4531): 353-361.

[169]

Kreisa R D, 1981. Storm-generated sedimentary structures in subtidal marine facies with examples from the Middle and Upper Ordovician of southwestern Virginia[J]. Journal of Sedimentary Research, 51(3): 823-848.

[170]

Kuenen P H, Migliorini C I, 1950. Turbidity currents as a cause of graded bedding[J]. The Journal of Geology, 58(2): 91-127.

[171]

Labourdette R, 2007. Integrated three-dimensional modeling approach of stacked turbidite channels[J]. AAPG Bulletin, 91(11): 1603-1618.

[172]

Lara F, Lara-Cueva R, Larco J C, et al., 2021. A deep learning approach for automatic recognition of seismo-volcanic events at the Cotopaxi volcano[J]. Journal of Volcanology and Geothermal Research, 409: 107142.

[173]

Leenman A S, Eaton B C, Mackenzie L G, 2022. Floods on allu-vial fans:implications for reworking rates,morphology and fan hazards[J]. Journal of Geophysical Research: Earth Surface, 127(2): e2021JF006367.

[174]

Li J J, Jansen J D, Carling P A, et al., 2025a. Palaeoseismicity recorded in soft-sediment deformation structures within a 166-m-long drill core from Diexi Palaeolake,eastern Tibetan Plateau[J]. Journal of Mountain Science, 22(12): 4464-4489.

[175]

Li F J, Chen Z A, Acikalin S, et al., 2025b. Storm deposit charac-teristics and orbital cyclicity of the Early Devonian Xiejia wan Formation in the Longmenshan area, Sichuan Province, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecol-ogy, 664: 112792.

[176]

Maier K L, Strachan L J, Tickle S, et al., 2024. Testing turbidite conceptual models with the Kaikōura Earthquake co-seismic event bed,Aotearoa New Zealand[J]. Journal of Sedimen-tary Research, 94(3): 325-333.

[177]

Magirl C S, Griffiths P G, Webb R H, 2010. Analyzing debris flows with the statistically calibrated empirical model LAHARZ in southeastern Arizona,USA[J]. Geomorphology, 119(1/2): 111-124.

[178]

Manville V, Németh K, Kano K, 2009. Source to sink:a review of three decades of progress in the understanding of volcani-clastic processes, deposits, and hazards[J]. Sedimentary Geology, 220(3/4): 136-161.

[179]

Liao Z W, Hu W X, Cao J, et al., 2020. Oceanic anoxia through the late Permian Changhsingian Stage in the Lower Yangtze region,South China:evidence from sulfur isotopes and trace elements[J]. Chemical Geology, 532: 119371.

[180]

Middleton G V, Hampton M A, 1973. Sediment gravity flows:mechanics of flow and deposition[C]// Middleton G V, Bouma A H. Turbidity Currents and Deep-Water Sedimenta-tion. Los Angeles:Pacific Section SEPM: 1-38.

[181]

Modie B N, 2002. A glacigenic interpretation of a Neoarchaean (≈2.78 Ga) volcanogenic sedimentary sequence in the Nnywane Formation,Sikwane,Southeast Botswana[J]. Jour-nal of African Earth Sciences, 35(1): 163-175.

[182]

Molenaar A, Wils K, Van Daele M, et al., 2024. Shaken and stirred: a comparative study of earthquake-triggered soft-sediment deformation structures in lake sediments[J]. Geochemistry, Geophysics, Geosystems, 25(6): e2023-GC011402.

[183]

Montenat C, Barrier P,Ott d’estevou P, et al., 2007. Seismites:an attempt at critical analysis and classification[J]. Sedimentary Geology, 196(1/2/3/4): 5-30.

[184]

Moretti M, Pieri P, Tropeano M, 2002. Late Pleistocene soft-sediment deformation structure interpreted as seismites in paralic deposits in the city of Bari (Apulian foreland,south-ern Italy)[J]. Special Paper of the Geological Society of America, 359: 75-85.

[185]

Owen G, 1996. Experimental soft-sediment deformation: struc-tures formed by the liquefaction of unconsolidated sands and some ancient examples[J]. Sedimentology, 43(2): 279-293.

[186]

Patacci M, Marini M, Felletti F, et al., 2020. Origin of mud in turbidites and hybrid event beds: insight from ponded mudstone caps of the Castagnola turbidite system (north-west Italy)[J]. Sedimentology, 67(5): 2625-2644.

[187]

Percival L M E, van Helmond N A G M, Selby D, et al., 2020. Complex interactions between large igneous province emplacement and global-temperature changes during the Cenomanian-Turonian oceanic anoxic event (OAE 2)[J]. Paleoceanography and Paleoclimatology, 35(10): e2020-PA004016.

[188]

Rodrı́guez-Pascua M A, Calvo J P, De Vicente G, et al., 2000. Soft-sediment deformation structures interpreted as seis-mites in lacustrine sediments of the Prebetic Zone, SE Spain, and their potential use as indicators of earthquake magnitudes during the Late Miocene[J]. Sedimentary Geol-ogy, 135(1/2/3/4): 117-135.

[189]

Rogov M A, Shchepetova E V, Zakharov V A, 2020. Late Juras-sic-earliest Cretaceous prolonged shelf dysoxic-anoxic event and its possible causes[J]. Geological Magazine, 157(10): 1622-1642.

[190]

Savelyeva O L, 2019. Geochemical events at the Cenomanian-Turonian boundary: relation of anoxia with volcanism,climate, and ocean circulation[J]. Russian Geology and Geophysics, 60(9): 990-1007.

[191]

Schlanger S O, Jenkyns H C, 1976. Cretaceous oceanic anoxic events:causes and consequences[J]. Geologie en Mijnbouw, 55(3/4): 179-184.

[192]

Schnyder J, Baudin F, Deconinck J F, 2005. A possible tsunami deposit around the Jurassic-Cretaceous boundary in the Boulonnais area (northern France)[J]. Sedimentary Geology, 177(3/4): 209-227.

[193]

Seilacher A, 1969. Fault-graded beds interpreted as seismites[J]. Sedimentology, 13(1/2): 155-159.

[194]

Shan X, Yu X H, Jin L N, et al., 2021. Bed type and flow mecha-nism of deep water sub-lacustrine fan fringe facies:an exam-ple from the Middle Permian Lucaogou Formation in South-ern Junggar Basin of NW China[J]. Petroleum Science, 18(2): 339-361.

[195]

Shanmugam G, 2000. 50 years of the turbidite paradigm (1950s-1990s): deep-water processes and facies models-a critical perspective[J]. Marine and Petroleum Geology, 17(2): 285-342.

[196]

Shimada Y, Matsumoto D, Tanigawa K, et al., 2025. Sedimento-logical and micropaleontological characteristics of tsunami deposits associated with the 2024 Noto Peninsula earth-quake[J]. Scientific Reports, 15(1): 9820.

[197]

Shinozaki T, Iguchi A, Nishijima M, et al., 2025. Identification of deposits from modern and ancient large tsunamis by means of environmental DNA[J]. Scientific Reports, 15(1): 242.

[198]

Sun W W,Ming G D,Yang G M, et al., 2026. 41Ca exposure dating of glacial moraines[J/OL]. Science Bulletin, 2026-03-24. https://doi.org/10.1016/j.scib.2026.03.052.

[199]

Talling P J, 2014. On the triggers, resulting flow types and frequencies of subaqueous sediment density flows in differ-ent settings[J]. Marine Geology, 352: 155-182.

[200]

Talling P J, Masson D G, Sumner E J, et al., 2012. Subaqueous sediment density flows:depositional processes and deposit types[J]. Sedimentology, 59(7): 1937-2003.

[201]

Tasistro-Hart A R, Macdonald F A, Crowley J L, et al., 2025. Four-million-year Marinoan snowball shows multiple routes to deglaciation[J]. Proceedings of the National Academy of Sciences of the United States of America, 122(18): e2418281122.

[202]

Walker R G, 1978. Deep-water sandstone facies and ancient submarine fans: models for exploration for stratigraphic traps[J]. AAPG Bulletin, 62(6): 932-966.

[203]

Wall S, Murphy B P, Belmont P, et al., 2023. Predicting post-fire debris flow grain sizes and depositional volumes in the Inter-mountain West, United States[J]. Earth Surface Processes and Landforms, 48(1): 179-197.

[204]

Westermann S, Vance D, Cameron V, et al., 2014. Heterogeneous oxygenation states in the Atlantic and Tethys oceans during oceanic anoxic event 2[J]. Earth and Planetary Science Letters, 404: 178-189.

[205]

Wignall P B, Twitchett R J, 1996. Oceanic anoxia and the end Permian mass extinction[J]. Science, 272(5265): 1155-1158.

[206]

Wilhelm B, Amann B, Corella J P, et al., 2022. Reconstructing paleoflood occurrence and magnitude from lake sediments[J]. Quaternary, 5(1): 9.

[207]

Yang T, Cao Y C, Liu K Y, et al., 2019. Origin of deep-water fine-grained sediments as revealed from the Lower Cretaceous rifting basin sequence in the Lingshan Island,Yellow Sea, eastern China[J]. Journal of Asian Earth Sciences, 186: 104065.

[208]

Young G M, 1991. The geologic record of glaciation:relevance to the climatic history of Earth[J]. Geoscience Canada, 18(3): 100.

[209]

Yu X X, Bai J H, Wei G J, et al., 2026. Stable neodymium isotopic composition of the upper continental crust through time from ancient glacial diamictites and Holocene marine sedi-ments[J]. Geochimica et Cosmochimica Acta, 422: 235-246.

[210]

Zhang T S, Kershaw S, Wan Y, et al., 2000. Geochemical and facies evidence for palaeoenvironmental change during the Late Ordovician Hirnantian glaciation in South Sichuan Province, China[J]. Global and Planetary Change, 24(2): 133-152.

[211]

Zhao X D, Xue N H, Yang H, et al., 2025. Climate-carbon-cycle interactions and spatial heterogeneity of the late Triassic Carnian pluvial episode[J]. Nature Communications, 16: 5404.

[212]

Zhong G F, Cartigny M J B, Kuang Z G, et al., 2015. Cyclic steps along the South Taiwan Shoal and West Penghu submarine canyons on the northeastern continental slope of the South China Sea[J]. Geological Society of America Bulletin, 127(5/6): 804-824.

[213]

Zurli L, Perotti M, Cornamusini G, 2024. Composition of Late Paleozoic Ice Age tillites in Victoria Land (Antarctica):implications for sediment provenance and ice centers extent in southern Gondwana[J]. Rendiconti Online della Società Geologica Italiana, 63: 37-44.

基金资助

国家自然科学基金项目(42372141, 42172135)

国家十三五科技重大专项(2016ZX05046-005-01)

国家十五五科技重大专项(2025ZD1400204)

AI Summary AI Mindmap
PDF (6281KB)

0

访问

0

被引

详细

导航
相关文章

AI思维导图

/

〈 〉