东非鲁伍马盆地海底峡谷发育特征及成因机制

doi:10.11885/j.issn.1674-5086.2024.08.28.07

西南石油大学学报(自然科学版) ›› 2025, Vol. 47 ›› Issue (1): 67-79.DOI: 10.11885/j.issn.1674-5086.2024.08.28.07

• 深海油气勘探与开发地质专刊 • 上一篇下一篇

东非鲁伍马盆地海底峡谷发育特征及成因机制

马宏霞¹, 朱越越², 许小勇¹, 何云龙², 王红平¹

1. 中国石油杭州地质研究院, 浙江杭州 310023;
2. 中国地质大学(武汉) 海洋地质资源湖北省重点实验室, 湖北武汉 430074

收稿日期:2024-08-28 发布日期:2025-03-12
通讯作者: 朱越越,E-mail:13734374932@163.com
作者简介:马宏霞，1985年生，女，汉族，江苏如皋人，高级工程师，硕士，主要从事深水沉积学与深水沉积油气勘探开发方面的研究工作。E-mail：mahx_hz@petrochina.com.cn
朱越越，1998年生，女，汉族，山东临沂人，硕士研究生，主要从事深水沉积学与深水沉积油气勘探开发方面的研究工作。E-mail：13734374932@163.com
许小勇，1983年，男，汉族，江苏无锡人，高级工程师，硕士，主要从事深水沉积油气勘探方面的研究工作。E-mail：xuxy_hz@petrochina.com.cn
何云龙，1983年生，男，汉族，湖北荆门人，副教授，博士，主要从事海洋地质、沉积盆地分析、沉积水动力学模拟及其相关石油（能源)地质方面的研究工作。E-mail：ylhe@cug.edu.cn
王红平，1982年生，男，汉族，四川自贡人，高级工程师，博士，主要从事深海油气勘探开发研究方面的研究工作。E-mail：wanghp_hz@petrochina.com.cn
基金资助:
国家自然科学基金（41502102，42072137)

Developmental Characteristics and Genesis Mechanisms of Submarine Canyons in the Rovuma Basin, East Africa

MA Hongxia¹, ZHU Yueyue², XU Xiaoyong¹, HE Yunlong², WANG Hongping¹

1. Hangzhou Research Institute of Petroleum Geology, PetroChina, Hangzhou, Zhejiang 310023, China;
2. Hubei Key Laboratory of Marine Geological Resources, China University of Geosciences (Wuhan) , Wuhan, Hubei 430074, China

Received:2024-08-28 Published:2025-03-12

摘要/Abstract

摘要： 针对鲁伍马盆地海底峡谷的发育特征和成因机制认识尚不全面，利用三维地震资料，结合深水沉积学的相关理论与前人研究成果，开展了对海底峡谷外部形态特征、内部充填结构和成因机制的研究。结果表明，研究区内鲁伍马盆地发育10个峡谷，整体呈东西走向；垂向上呈上游尖窄V形、下游宽缓U形特征，平面上呈孤立—合并—分散特征；峡谷内部充填沉积类型包括底部滞留沉积、滑塌及块体流搬运体沉积；峡谷外部可见漂积体、麻坑。结合研究区海底峡谷发育背景，认为其可能存在两种成因机制：一是由于下伏地层中天然气向上逃逸形成麻坑，造成地层薄弱易侵蚀，相邻麻坑串联沟通形成峡谷雏形，并在后期含沉积物流体改造与侵蚀下逐渐形成；二是由于下陆坡大型断层的活动导致下陆坡沉积物失稳，导致原始沉积层崩塌形成的重力流事件，在重力流侵蚀作用下而形成。

关键词: 鲁伍马盆地, 海底峡谷, 地貌特征, 沉积特征, 成因机制

Abstract: The external morphological characteristics, internal filling structure and genetic mechanism of submarine canyons in the Rovuma Basin are not fully understood. We make a study on the external morphological characteristics, internal filling structure and genetic mechanism of submarine canyons by using three-dimensional seismic data, combined with the relevant theories of deep-water sedimentology and previous research results. The results indicate that there are 10 canyons in the Rovuma Basin, trending east-west, with a V-shaped narrow upstream and U-shaped gentle downstream profile vertically, and showing an isolated-merged-dispersed pattern on the horizontal plane. The internal filling sediment types in the canyons include basal lags, slides and MTDs. Outside the canyons, sediment drifts and pockmarks are observed. Considering the developmental background of submarine canyons in the study area, it is believed that there may be two genesis mechanisms at play. One involves the escape of natural gas from the underlying strata, leading to the formation of pockmarks and subsequent erosion of weak layers, with interconnected pockmarks forming the initial shape of the canyon, gradually evolving under the influence of sediment-laden fluid flow and erosion. The second mechanism involves destabilization of sediment on the lower slope due to the activity of large-scale faults, resulting in gravity flow events and subsequent erosion leading to canyon formation.

Key words: Rovuma Basin, submarine canyons, geomorphological features, sedimentary characteristics, genetic mechanisms

中图分类号:

TE121
P737.2

马宏霞, 朱越越, 许小勇, 何云龙, 王红平. 东非鲁伍马盆地海底峡谷发育特征及成因机制[J]. 西南石油大学学报(自然科学版), 2025, 47(1): 67-79.

MA Hongxia, ZHU Yueyue, XU Xiaoyong, HE Yunlong, WANG Hongping. Developmental Characteristics and Genesis Mechanisms of Submarine Canyons in the Rovuma Basin, East Africa[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2025, 47(1): 67-79.

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参考文献

[1] 韩喜彬,李家彪,龙江平,等.我国海底峡谷研究进展[J].海洋地质动态, 2010, 26(2): 41-48. doi:10.396 9/j.issn.1009-2722.2010.02.007 HAN Xibin, LI Jiabiao, LONG Jiangping, et al. Development of research on submarine canyon in China[J]. Marine Geology Frontiers, 2010, 26(2): 41-48. doi:10.3969/j.issn.1009-2722.2010.02.007
[2] 杜文波,聂鑫,杨楚鹏,等.南海北部珠江口外峡谷体系沉积特征、演化及其控制因素[J].地球科学, 2022, 47(11): 4046-4059. doi:10.3799/dqkx.2022.166 DU Wenbo, NIE Xin, YANG Chupeng, et al. Sedimentary characteristics, evolution and controlling factors of the pearl river canyon system in the northern South China Sea[J]. Editorial Committee of Earth Science-Journal of China University of Geosciences, 2022, 47(11): 4046-4059. doi:10.3799/dqkx.2022.166
[3] SHEPARD F P, CURRAY J R, INMAN D L, et al. Submarine geology by diving saucer:Bottom currents and precipitous submarine canyon walls continue to a depth of at least 300 meters[J]. Science, 1964, 3636(145): 1042-1046. doi:10.1126/science.145.3636.1042
[4] PICKERING K, STOW D, WATSON M, et al. Deep-water facies, processes and models:A review and classification scheme for modern and ancient sediments[J]. EarthScience Reviews, 1986, 23:75-174. doi:10.1016/0012-82 52(86) 90001-2
[5] 陈奎,王雯娟,徐万兴,等.琼东南盆地中央峡谷深海一号"大气田周缘成藏条件与滚动勘探成效[J].石油实验地质, 2023, 45(5): 994-1006. doi: 10.11781/sysydz202305994 CHEN Kui, WANG Wenjuan, XU Wanxing, et al. Accumulation conditions and rolling exploration results in the periphery "Deep sea No. 1" giant gas field in central canyon of Qiongdongnan Basin[J]. Petroleum Geology and Experiment, 2023, 45(5): 994-1006. doi:10.11781/sysydz 202305994
[6] 刘静静,刘震,王子嵩,等.琼东南盆地深水区中央峡谷天然气藏输导模式研究[J].石油实验地质, 2019, 41(2): 193-199. doi:10.11781/sysydz201902193 LIU Jingjing, LIU Zhen, WANG Zisong, et al. Gas migration mode for the central canyon in deep-water Qiongdongnan Basin[J]. Petroleum Geology and Experiment, 2019, 41(2): 193-199. doi:10.11781/sysydz201902193
[7] LEWIS K B, BARNES P M. Kaikoura Canyon, New Zealand:Active conduit from near-shore sediment zones to trench-axis channel[J]. Marine Geology, 1999, 162(1): 39-69. doi:10.1016/S0025-3227(99) 00075-4
[8] HARRIS P T, WHITEWAY T. Global distribution of large submarine canyons:Geomorphic differences between active and passive continental margins[J]. Marine Geology, 2011, 285(1-4): 69-86. doi:10.1016/j.margeo.2011.05.008
[9] 陈奎,胡德胜,宋瑞有,等.深水中大型气田滚动勘探技术体系与成效——以琼东南盆地中央峡谷A边际气田为例[J].石油实验地质, 2024, 46(1): 1-10. doi: 10.11781/sysydz202401001 CHEN Kui, HU Desheng, SONG Ruiyou, et al. Technical system and achievements of rolling exploration in large and medium-sized deep-water gas fields[J]. Petroleum Geology&Experiment, 2024, 46(1): 1-10. doi:10.11781/sysydz202401001
[10] PICKERING K T, STOW D A. Inorganic major, minor, and trace element geochemistry and clay mineralogy of sediments from the deep sea drilling project Leg 96, Gulf of Mexico[J]. Research, 1986, 96:733-745. doi:10.2973/dsdp.proc.96.144.1986
[11] 陈建宏,栾锡武,魏新元.安达曼海东部丹老陆坡峡谷群沉积演化过程及成因探讨[J/OL].沉积学报.[2022-05-20]. https://doi.org/10.14027/j.issn.1000-0550.2022.052. doi:10.14027/j.issn.1000-0550.2022.052 CHEN Jianhong, LUAN Xiwu, WEI Xinyuan. Discussion on the sedimentary evolution process and genesis of Dangui slope canyon group in eastern Andaman Sea[J]. Acta Sedimentologica Sinica.[2022-05-20]. https://doi.org/10.14027/j.issn.1000-0550.2022.052. doi:10.14027/j.issn.1000-0550.2022.052
[12] 刘巍,胡林,廖仪,等.陵水凹陷中央峡谷水道砂体构型地震响应正演模拟及有利分布区预测[J].中国海上油气, 2020, 32(6): 43-53. doi:10.11935/j.issn.1673-1506.2020.06.005 LIU Wei, HU Lin, LIAO Yi, et al. Forward simulation on seismic response of channel sand body architecture in central canyon of Lingshui Sag and favorable zone prediction[J]. China Offshore Oil and Gas, 2020, 32(6): 43-53. doi:10.11935/j.issn.1673-1506.2020.06.005
[13] MAIER K L, JOHNSON S Y, HART P. Controls on submarine canyon head evolution:Monterey Canyon, offshore central California[J]. Marine Geology, 2018, 404: 24-40. doi:10.1016/j.margeo.2018.06.014
[14] JOBE Z R, LOWE D R, UCHYTIL S J. Two fundamentally different types of submarine canyons along the continental margin of equatorial guinea[J]. Marine and Petroleum Geology, 2011, 28(3): 843-860. doi:10.1016/j.marpetgeo.2010.07.012
[15] SUSANTH S, KURIAN P J, BIJESH C M, et al. Controls on the evolution of submarine canyons in steep continental slopes:Geomorphological insights from Palar Basin, southeastern margin of India[J]. Geo-Marine Letters, 2021, 41:14. doi:10.1007/s00367-021-00685-9
[16] NARANJO-VESGA J, PANIAGUA-ARROYAVE J F, ORTIZ-KARPF A, et al. Controls on submarine canyon morphology along a convergent tectonic margin the southern Caribbean of Colombia[J]. Marine and Petroleum Geology, 2022, 137:105493. doi:10.1016/j.marpetgeo.2021.105493
[17] 赵月霞,刘保华,李西双,等.东海陆坡海底峡谷扇体系沉积特征及物质搬运[J].古地理学报, 2011, 13(1): 119-126. ZHAO Yuexia, LIU Baohua, LI Xishuang, et al. Sedimentary characters and material transportation of submarine canyon-fan systems in slope of the East China Sea[J]. Journal of Palaeogeography, 2011, 13(1): 119-126.
[18] 殷绍如,王嘹亮,郭依群,等.东沙海底峡谷的地貌沉积特征及成因[J].中国科学(地球科学), 2015, 45(3): 275-289. doi:10.1007/s11430-014-5044-8 YIN Shaoru, WANG Liaoliang, GUO Yiqun, et al. Morphology, sedimentary characteristics, and origin of the Dongsha submarine canyon in the northeastern continental slope of the South China Sea[J]. Scientia Sinica (Terrae), 2015, 45(3): 275-289. doi:10.1007/s11430-014-5044-8
[19] 徐尚,王英民,彭学超,等.台湾峡谷的成因及其对沉积的控制[J].中国科学(地球科学), 2014, 44(9): 1913-1924. doi:10.1007/s11430-014-4942-0 XU Shang, WANG Yingmin, PENG Xuechao, et al. Origin of Taiwan Canyon and its effects on deepwater sediment[J]. Scientia Sinica (Terrae), 2014, 44(9): 1913-1924. doi:10.1007/s11430-014-4942-0
[20] 孙美静,高红芳,李学杰.台湾东部海域台东峡谷沉积特征及其成因[J].地球科学, 2018, 43(10): 3709-3718. doi:10.3799/dqkx.2017.515 SUN Meijing, GAO Hongfang, LI Xuejie. Sedimentary characteristics and origin of Taitung Canyon in eastern waters of Taiwan Island[J]. Earth Science, 2018, 43(10): 3709-3718. doi:10.3799/dqkx.2017.515
[21] 朱林,傅命佐,刘乐军,等.南海北部白云凹陷陆坡海底峡谷地形地貌与沉积地层特征[J].海洋地质与第四纪地质, 2014, 34(2): 1-9. doi:10.3724/SP. J.1140.2014.02001 ZHU Lin, FU Mingzuo, LIU Lejun, et al. Topographic and sedimentary stratigraphic characteristics of submarine canyon on the slope of Baiyun Sag in the northern South China Sea[J]. Marine Geology&Quaternary Geology, 2014, 34(2): 1-9. doi:10.3724/SP.J.1140.2014.02001
[22] 王星星,蔡峰,孙治雷,等.南海北部东沙海底峡谷沉积演化过程及其地质意义[J].地球科学, 2021, 46(3): 1023-1037. doi:10.3799/dqkx.2020.277 WANG Xingxing, CAI Feng, SUN Zhilei, et al. Sedimentary evolution and geological significance of the Dongsha submarine canyon in the northern South China Sea[J]. Earth Science, 2021, 46(3): 1023-1037. doi:10.3799/dqkx.2020.277
[23] 张青林,张向涛,李洪博,等.南海北部狭窄陆架断裂陆坡控制的大型深水扇体系[J].地球科学, 2022, 47(7): 2421-2432. doi:10.3799/dqkx.2022.157 ZHANG Qinglin, ZHANG Xiangtao, LI Hongbo, et al. Large submarine fan system controlled by narrow continental shelf-faulted continental slope in northern South China Sea[J]. Earth Science, 2022, 47(7): 2421-2432. doi: 10.3799/dqkx.2022.157
[24] 田洁,宋军,马本俊,等.中建海底峡谷地貌及沉积特征的分段性[J].地球科学, 2021, 46(2): 708-718. doi: 10.3799/dqkx.2020.062 TIAN Jie, SONG Jun, MA Benjun, et al. Segmentation features of geomorphology and sedimentary structure of Zhongjian Canyon[J]. Earth Science, 2021, 46(2): 708-718. doi:10.3799/dqkx.2020.062
[25] 裴健翔,宋鹏,郭明刚,等.琼东南盆地第四纪中央峡谷体系沉积演化与油气前景[J].地球科学, 2023, 48(2): 451-464. doi:10.3799/dqkx.2022.487 PEI Jianxiang, SONG Peng, GUO Minggang, et al. Sedimentary evolution and hydrocarbon exploration prospect of the quaternary central canyon system in the Qiongdongnan Basin[J]. Earth Science, 2023, 48(2): 451-464. doi: 10.3799/dqkx.2022.487
[26] 于星,赵红岩,邱春光,等.东非海岸盆地第四系深水沉积特征、过程及沉积模式[J].断块油气田, 2024, 31(2): 257-265. doi:10.6056/dkyqt202402010 YU Xing, ZHAO Hongyan, QIU Chunguang, et al. Quaternary deep-water deposition in coastal basins of East Africa:Characteristics, processes, and depositional model[J]. Fault-Block Oil and Gas Field, 2024, 31(2): 257-265. doi:10.6056/dkyqt202402010
[27] 孙辉,范国章,王红平,等.东非鲁伍马盆地中始新统深水沉积特征及层序界面识别方法[J].岩性油气藏, 2023, 35(6): 106-116. doi:10.12108/yxyqc.20230612 SUN Hui, FAN Guozhang, WANG Hongping, et al. Deepwater sedimentary characteristics and sequence boundary identification of Middle Eocene in Rovuma Basin, East Africa[J]. Lithologic Reservoirs, 2023, 35(6): 106-116. doi:10.12108/yxyqc.20230612
[28] 陈宇航,姚根顺,吕福亮,等.东非鲁伍马盆地渐新统深水水道朵体沉积特征及控制因素[J].石油学报, 2017, 38(9): 1047 1058. doi:10.7623/syxb201709006 CHEN Yuhang, YAO Genshun, LÜ Fuliang, et al. Sedimentary characteristics and controlling factors of Oligocene deep-water channel-lobe in Rovuma Basin of the East Africa[J]. Acta Petrolei Sinica, 2017, 38(9): 1047-1058. doi:10.7623/syxb201709006
[29] 曹全斌,鲁银涛,陈宇航,等.东非鲁伍马盆地下始新统深水沉积储层特征及沉积演化[J].海相油气地质, 2022, 27(4): 396-404. doi:10.3969/j.issn.1672-9854.2022.04.006 CAO Quanbin, LU Yintao, CHEN Yuhang, et al. Reservoir characteristics and sedimentary evolution of deep water deposition of Lower Eocene in Rovuma Basin, East Africa[J]. Marine Origin Petroleum Geology, 2022, 27(4): 396-404. doi:10.3969/j.issn.1672-9854.2022.04.006
[30] 张佳佳,吴胜和,王瑞峰,等.东非鲁伍马盆地深水X 气藏海底扇储层构型研究:重力流底流交互作用的指示意义[J].古地理学报, 2023, 25(1): 163-179. doi: 10.7605/gdlxb.2023.01.011 ZHANG Jiajia, WU Shenghe, WANG Ruifeng, et al. Submarine-fan reservoir architecture of deepwater Gasfield X in Rovuma Basin offshore East Africa:Insights for the interaction between sediment gravity flows and bottom currents[J]. Journal of Palaeogeography, 2023, 25(1): 163-179. doi:10.7605/gdlxb.2023.01.011
[31] 孔祥宇.东非鲁武马盆地油气地质特征与勘探前景[J]. 岩性油气藏, 2013, 25(3): 21-27. doi:10.3969/j.issn.1673-8926.2013.03.004 KONG Xiangyu. Petroleum geologic characteristics and exploration prospect in Rovuma Basin, East Africa[J]. Lithologic Reservoirs, 2013, 25(3): 21-27. doi:10.3969/j.issn.1673-8926.2013.03.004
[32] 曹全斌,唐鹏程,吕福亮,等.东非鲁伍马盆地深水浊积砂岩气藏成藏条件及控制因素[J].海相油气地质, 2018, 23(3): 65-72. doi:10.3969/j.issn.1672-9854.2018.03.007 CAO Quanbin, TANG Pengcheng, LÜ Fuliang, et al. Formation conditions and controlling factors of gas-bearing turbidite sand reservoirs in deep water deposits in the Rovuma Basin, East Africa[J]. Marine Origin Petroleum Geology, 2018, 23(3): 65-72. doi:10.3969/j.issn.1672-9854.2018.03.007
[33] 张光亚,刘小兵,赵健,等.东非被动大陆边缘盆地演化及大气田形成主控因素:以鲁武马盆地为例[J].地学前缘, 2018, 25(2): 24-32. doi:10.13745/j.esf.2018.02.003 ZHANG Guangya, LIU Xiaobing, ZHAO Jian, et al. Passive continental margin basin evolution of East Africa and the main controlling factors of giant gas fields:An example from the Rovuma Basin[J]. Earth Science Frontiers, 2018, 25(2): 24-32. doi:10.13745/j.esf.2018.02.003
[34] 刘子玉,吕明,卢景美,等.东非鲁伍马盆地窄陆架背景下的深水沉积体系[J].海相油气地质, 2017, 22(4): 27-34. doi:10.3969/j.issn.1672-9854.2017.04.004 LIU Ziyu, LÜ Ming, LU Jingmei, et al. Deepwater depositional system in the background of narrow shelf in the Ruvuma Basin, eastern Africa[J]. Marine Origin Petroleum Geology, 2017, 22(4): 27-34. doi:10.3969/j.issn.1672-9854.2017.04.004
[35] 李华,梁建设,邱春光,等.东非海岸重点盆地渐新世构造事件沉积体系耦合关系研究[J].地质学报, 2022, 96(5): 1855-1867. doi:10.3969/j.issn.0001-5717.2022.05.021 LI Hua, LIANG Jianshe, QIU Chunguang, et al. The relationship between tectonic events and sedimentary systems in coastal key basins of the East Africa[J]. Acta Geologica Sinica, 2022, 96(5): 1855-1867. doi:10.3969/j.issn.0001-5717.2022.05.021
[36] FUHRMANN A, KANE I A, CLARE M A, et al. Hybrid turbidite-drift channel complexes:An integrated multiscale model[J]. Geology, 2020, 48(6): 562-568. doi:10.1130/G47179.1
[37] STOW D, SMILLIE. Z. Distinguishing between deepwater sediment facies:Turbidites, contourites and hemipelagites[J]. Geosciences, 2020, 10(2): 68. doi:10.3390/geo sciences10020068
[38] 苏明,王艺璇,陈慧,等.南海北部中深层环流格局下海山阶地峡谷沉积效应[J].海洋地质与第四纪地质, 2023, 43(3): 61 73. doi:10.16562/j.cnki.0256-1492.2023052201 SU Ming, WANG Yixuan, CHEN Hui, et al. Depositional mode for the seamount-terrace-canyon sedimentary combination under the impacts of intermediate and deep circulation dynamics in the northern margin of the South China Sea[J]. Marine Geology&Quaternary Geology, 2023, 43(3): 61-73. doi:10.16562/-j.cnki.0256-1492.202305-2201
[39] 张笑,王振奇,李士涛,等.下刚果盆地深水沉积中新统层序划分及其控制因素[J].海洋地质前沿, 2011, 27(10): 27-33. doi:10.16028/j.1009-2722.2011.10.003 ZHANG Xiao, WANG Zhenqi, LI Shitao, et al. Sequence stratigraphy of the deepwater miocene in the lower Congo Basin and its controlling factors[J]. Marine Geology Frontiers, 2011, 27(10): 27-33. doi:10.16028/j.1009-2722.2011.10.003
[40] 孙辉,唐鹏程,陈宇航,等.东非鲁武马盆地陆坡深水沉积特征及主控因素[J].海洋地质与第四纪地质, 2016, 36(3): 59-68. doi:10.16562/j.cnki.0256-1492.2016.03.006 SUN Hui, TANG Pengcheng, CHEN Yuhang, et al. Characteristics and controlling factors of deepwater deposits on the continental slope of the Rovuma Basin, East Africa[J]. Marine Geology&Quaternary Geology, 2016, 36(3): 59-68. doi:10.16562/j.cnki.0256-1492.2016.03.006
[41] 孙美静,姚永坚,罗伟东,等.南海西北部中建南海底峡谷群的发现及演化特征[J].地球科学, 2022, 47(11): 4005-4019. doi:10.3799/dqkx.2022.034 SUN Meijing, YAO Yongjian, LUO Weidong, et al. Sedimentary evolution characteristics and controlling factors of Zhongjiannan Canyons in northwestern South China Sea[J]. Earth Science, 2022, 47(11): 4005-4019. doi:10.3799/dqkx.2022.034
[42] 刘钰星,陈宇航,范国章,等.底流与重力流交互作用下的朵体沉积特征:以东非鲁伍马盆地中新统为例[J].古地理学报, 2024, 26(4): 1005-1016. doi: 10.7605/gdlxb.2024.00.054 LIU Yuxing, CHEN Yuhang, FAN Guozhang, et al. Sedimentary characteristics of lobes formed by interacting bottom currents and gravity flows:A case study from the Miocene in Rovuma Basin, East Africa[J]. Journal of Palaeogeography, 2024, 26(4): 1005-1016. doi:10.7605/gdlxb.2024.00.054
[43] 薛国庆,张辉,潘燕,等.琼东南盆地A区块中新统黄流组中央峡谷充填演化[J].中国海上油气, 2023, 35(4): 35-46. doi:10.11935/j.issn.1673-1506.2023.04.004 XUE Guoqing, ZHANG Hui, PAN Yan, et al. Filling evolution of central canyon in Huangliu Formation of Miocene in Block A of Qiongdongnan Basin[J]. China Offshore Oil and Gas, 2023, 35(4): 35-46. doi:10.11935/j.issn.1673-1506.2023.04.004
[44] 王长盛,朱俊江,赵冬冬,等.全球海底峡谷成因及演化研究[J].海洋地质前沿, 2021, 37(3): 1-15. doi: 10.16028/j.1009-2722.2020.119 WANG Zhangsheng, ZHU Junjiang, ZHAO Dongdong, et al. Origin and evolution of submarine canyons[J]. Marine Geology Frontiers, 2021, 37(3): 1-15. doi:10.-16028/j.1009-2722.2020.119
[45] 李林,曲永强,孟庆任,等.重力流沉积:理论研究与野外识别[J].沉积学报, 2011, 29(4): 677-688. doi: 10.14027/j.cnki.cjxb.2011.04.019 LI Lin, QU Yongqiang, MENG Qingren, et al. Gravity flow sedimentation:Theoretical studies and field identification[J]. Acta Sedimentologica Sinica, 2011, 29(4): 677-688. doi:10.14027/j.cnki.cjxb.2011.04.019
[46] KLAUCKE I, MASSON D G, KENYON N H, et al. Sedimentary processes of the Lower Monterey Fan Channel and channel-mouth lobe[J]. Marine Geology, 2004, 206(1-4): 181-198. doi:10.1016/j.margeo.2004.02.006
[47] MILLER K G, KOMINZ M A, BROWNING J V, et al. The phanerozoic record of global sea-level change[J]. Science, 2005, 310(5752): 1293-1298. doi:10.1126/science.1116412
[48] 陈宇航,姚根顺,吕福亮,等.东非鲁伍马盆地深水区构造-沉积演化过程及油气地质特征[J].海相油气地质, 2016, 21(2): 39-46. doi:10.3969/j.issn.1672-9854.2016.02.005 CHEN Yuhang, YAO Genshun, LÜ Fuliang, et al. Tectonic-sedimentary evolution and petroleum geology characteristics in deepwater area in Rovuma Basin, East Africa[J]. Marine Origin Petroleum Geology, 2016, 21(2): 39-46. doi:10.3969/j.issn.1672-9854.2016.02.005
[49] 陈宇航,姚根顺,邵大力,等.坦桑尼亚滨海盆地陆坡峡谷沉积特征及其控制因素[J].古地理学报, 2021, 23(6): 1158-1173. doi:10.7605/gdlxb.2021.06.074 CHEN Yuhang, YAO Genshun, SHAO Dali, et al. Sedimentary characteristics and its controlling factors of continental slope canyons in Tanzania Coastal Basin[J]. Journal of Palaeogeography, 2021, 23(6): 1158-1173. doi:10.760 5/gdlxb.2021.06.074
[50] DE RUIJTER W P M, RIDDERINKHOF H, JOHANN R E, et al. Observations of the flow in the Mozambique Channel[J]. Geophysical Research Letters, 2002, 29(10): 140-143. doi:10.1029/2001GL013714
[51] 吴嘉鹏,王英民,王海荣,等.深水重力流与底流交互作用研究进展[J].地质论评, 2012, 58(6): 1110 1120. doi:10.16509/j.georeview.2012.06.007 WU Jiapeng, WANG Yingmin, WANG Hairong, et al. The interaction between deep-water turbidity and bottom currents:A review[J]. Geological Review, 2012, 58(6): 1110-1120. doi:10.16509/j.georeview.2012.06.007
[52] 李华,何幼斌.等深流沉积研究进展[J].沉积学报, 2017, 35(2): 228-240. doi:10.14027/j.cnki.cjxb.2017. 02.003 LI Hua, HE Youbin. Research processes on contourites[J]. Acta Sedimentologica Sinica, 2017, 35(2): 228-240. doi: 10.14027/j.cnki.cjxb.2017.02.003
[53] 龚承林,徐长贵,尤丽,等.深海重力流与底流交互作用的沉积响应及其勘探意义[J].矿物岩石地球化学通报, 2024, 43(4): 721-733. doi:10.3724/j.issn.1007-2802.20240025 GONG Chenglin, XU Zhanggui, YOU Li, et al. Depositional responses of the interaction between deep-marine gravity and bottom currents and their exploration significance[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2024, 43(4): 721-733. doi:10.3724/j.issn.1007--280 2.20240025
[54] SAID A, MODER C, CLARK S, et al. Sedimentary budgets of the Tanzania coastal basin and implications for uplift history of the East African rift system[J]. Journal of African Earth Sciences, 2015, 111:288-295. doi:10.1016/j.jafrearsci.2015.08.012
[55] 刘杰,苏明,乔少华,等.珠江口盆地白云凹陷陆坡限制型海底峡谷群成因机制探讨[J].沉积学报, 2016, 34(5): 940-950. doi:10.14027/j.cnki.cjxb.2016.05.013 LIU Jie, SU Ming, QIAO Shaohua, et al. Forming mechanism of the slope-confined submarine canyons in the Baiyun Sag, Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2016, 34(5): 940-950. doi:10.14027/j.cnki. cjxb.2016.05.013
[56] BANGS N L, HORNBACH M J, MOORE G F, et al. Massive methane release triggered by seafloor erosion offshore southwestern Japan[J]. Geology, 2010, 38(11): 1019-1022. doi:10.1130/G31491.1

东非鲁伍马盆地海底峡谷发育特征及成因机制

Developmental Characteristics and Genesis Mechanisms of Submarine Canyons in the Rovuma Basin, East Africa

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