Qingdao Institute of marine geology, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2022 Vol. 42, No. 5
Article Contents
Article navigation > Marine Geology & Quaternary Geology > 2022 > 42(5): 1-15
Next Article Previous Article

HU Gang, DU Xuexin, ZHU Wenjun, SHANG Luning, LI Panfeng, WEI Jia, MENG Yuanku, LEI Baohua, YU Yiyong, WANG Xiaojie. Progresses of ocean drilling in Bengal Fan: Scientific issues and drilling prospect[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 1-15. doi: 10.16562/j.cnki.0256-1492.2022061402
Citation: HU Gang, DU Xuexin, ZHU Wenjun, SHANG Luning, LI Panfeng, WEI Jia, MENG Yuanku, LEI Baohua, YU Yiyong, WANG Xiaojie. Progresses of ocean drilling in Bengal Fan: Scientific issues and drilling prospect[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 1-15. doi: 10.16562/j.cnki.0256-1492.2022061402
shu

Progresses of ocean drilling in Bengal Fan: Scientific issues and drilling prospect

  • 1.

    Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China

  • 2.

    Key Laboratory of Coastal Science and Integrated Management, Ministry of Natural Resources, Qingdao, 266061, China

  • 3.

    College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China

More Information
Received Date:  14 June 2022
Revised Date:  27 July 2022
Publish Date:  28 October 2022
    Abstract

  • The Bengal Fan is not only a source-sink transition zone connecting the plateau and the deep sea, but also an important product of plates drift and collision. Its deep sedimentary records are the natural archives of the India-Eurasia plate collision, the uplift and erosion process of the Qinghai Tibet Plateau and the evolution of climate and environment. We summarized the drilling expeditions and the latest research progress focusing on the sedimentary process and climate evolution since the late Miocene, the nature and evolution of the 90°E Ridge, and the formation of the South Asian monsoon in the Bengal Fan. However, constrained by drilling capacity and scientific targets, the full time sedimentary strata, the age and structural characteristics of the underlying oceanic crust in the Bengal Fan have not been effectively revealed which hinders the research on the long-time scale source to sink transition, the South Asia Mosoon formation and plate reconstruction. Based on the recently acquired high-quality multi-channel seismic data, the basement fluctuation, sedimentary structure and tectonic development characteristics of the Bengal Fan downstream are interpreted. Furthermore, we proposed three future scientific drilling locations which aim at the scientific drilling objectives including the complete sedimentary strata, age of oceanic crust basalt, and special structure characteristics. Well calibration and lithology prediction are carried out for these proposed drillings respectively. These proposed drillings are not only contributed to the reserve of scientific drilling for Chinese Ocean Drilling Vessel, but also significant for solving the frontier scientific issues of the Qinghai Tibet Plateau.

    • FullText(HTML)
  • 加载中
    • References
  • [1] 李江海, 程海艳, 赵星, 等. 残余洋盆的大地构造演化及其油气意义[J]. 地学前缘, 2009, 16(4):40-51 doi: 10.3321/j.issn:1005-2321.2009.04.005

    CrossRef Google Scholar

    LI Jianghai, CHENG Haiyan, ZHAO Xing, et al. Tectonic evolution of remnant oceanic basin and its implication for hydrocarbon [J]. Earth Science Frontiers, 2009, 16(4): 40-51. doi: 10.3321/j.issn:1005-2321.2009.04.005

    CrossRef Google Scholar

    [2] Curray J R, Emmel F J, Moore D G, et al. Structure, tectonics, and geological history of the Northeastern Indian Ocean[M]//Nairn A E M, Stehli F G. The Ocean Basins and Margins. Boston, MA: Springer, 1982: 399-450.

    Google Scholar

    [3] Royer J Y, Sandwell D T. Evolution of the eastern Indian Ocean since the Late Cretaceous: constraints from Geosat altimetry [J]. Journal of Geophysical Research:Solid Earth, 1989, 94(B10): 13755-13782. doi: 10.1029/JB094iB10p13755

    CrossRef Google Scholar

    [4] Lee T Y, Lawver L A. Cenozoic plate reconstruction of Southeast Asia [J]. Tectonophysics, 1995, 251(1-4): 85-138. doi: 10.1016/0040-1951(95)00023-2

    CrossRef Google Scholar

    [5] Talwani M, Desa M A, Ismaiel M, et al. The tectonic origin of the bay of Bengal and Bangladesh [J]. Journal of Geophysical Research:Solid Earth, 2016, 121(7): 4836-4851. doi: 10.1002/2015JB012734

    CrossRef Google Scholar

    [6] Curray J R, Emmel F J, Moore D G. The Bengal Fan: morphology, geometry, stratigraphy, history and processes [J]. Marine and Petroleum Geology, 2002, 19(10): 1191-1223. doi: 10.1016/S0264-8172(03)00035-7

    CrossRef Google Scholar

    [7] Curray J R. The Bengal depositional system: from rift to orogeny [J]. Marine Geology, 2014, 352: 59-69. doi: 10.1016/j.margeo.2014.02.001

    CrossRef Google Scholar

    [8] Alam M, Alam M M, Curray J R, et al. An overview of the sedimentary geology of the Bengal Basin in relation to the regional tectonic framework and basin-fill history [J]. Sedimentary Geology, 2003, 155(3-4): 179-208. doi: 10.1016/S0037-0738(02)00180-X

    CrossRef Google Scholar

    [9] Rowley D B, Currie B S. Palaeo-altimetry of the late Eocene to Miocene Lunpola basin, central Tibet [J]. Nature, 2006, 439(7077): 677-681. doi: 10.1038/nature04506

    CrossRef Google Scholar

    [10] Curray J R, Moore D G. Growth of the Bengal deep-sea fan and denudation in the Himalayas [J]. GSA Bulletin, 1971, 82(3): 563-572. doi: 10.1130/0016-7606(1971)82[563:GOTBDF]2.0.CO;2

    CrossRef Google Scholar

    [11] Peirce J W. The northward motion of India since the Late Cretaceous [J]. Geophysical Journal International, 1978, 52(2): 277-311. doi: 10.1111/j.1365-246X.1978.tb04234.x

    CrossRef Google Scholar

    [12] Duncan R A, Richards M A. Hotspots, mantle plumes, flood basalts, and true polar wander [J]. Reviews of Geophysics, 1991, 29(1): 31-50. doi: 10.1029/90RG02372

    CrossRef Google Scholar

    [13] Coffin M F, Pringle M S, Duncan R A, et al. Kerguelen hotspot magma output since 130 Ma [J]. Journal of Petrology, 2002, 43(7): 1121-1137. doi: 10.1093/petrology/43.7.1121

    CrossRef Google Scholar

    [14] Liu C S, Curray J R, McDonald J M. New constraints on the tectonic evolution of the eastern Indian Ocean [J]. Earth and Planetary Science Letters, 1983, 65(2): 331-342. doi: 10.1016/0012-821X(83)90171-1

    CrossRef Google Scholar

    [15] Radhakrishna M, Subrahmanyam C, Damodharan T. Thin oceanic crust below Bay of Bengal inferred from 3-D gravity interpretation [J]. Tectonophysics, 2010, 493(1-2): 93-105. doi: 10.1016/j.tecto.2010.07.004

    CrossRef Google Scholar

    [16] Curray J R. Sediment volume and mass beneath the Bay of Bengal [J]. Earth and Planetary Science Letters, 1994, 125(1-4): 371-383. doi: 10.1016/0012-821X(94)90227-5

    CrossRef Google Scholar

    [17] 李江海, 李洪林, 韩喜球. 印度洋底大地构造图[M]. 北京: 地质出版社, 2015

    Google Scholar

    LI Jianghai, LI Honglin, HAN Xiqiu. Tectonic Map of India Ocean[M]. Beijing: Geology Press, 2015.

    Google Scholar

    [18] Von Der Borch C C, Sclater J G, Gartner Jr S, et al. Initial reports of the deep sea drilling project, Volume 22[R]. Washington: U. S. Government Printing Office, 1974.

    Google Scholar

    [19] Cochran J R, Stow D A V. Proceedings of the ocean drilling program, initial report 116: Dital Bengal Fan[R]. College Station, TX, 1989.

    Google Scholar

    [20] Peirce J, Weissel J, Taylor E, et al. Proceedings of the ocean drilling program, initial report 121: Broken Ridge and NinetyEast Ridge[R]. College Station, TX: National Science Foundation, 1989.

    Google Scholar

    [21] Clemens S C, Kuhnt W, LeVay L J. Expedition 353 Scientific Prospectus: iMonsoon[R]. International Ocean Discovery Program, 2014.

    Google Scholar

    [22] Clemens S C, Kuhnt W, Levay L J. Expedition 353 preliminary report: Indian monsoon rainfall[R]. International Ocean Discovery Program, 2015.

    Google Scholar

    [23] Clemens S C, Kuhnt W, LeVay L J. Proceedings of the international ocean discovery Program 353: Indian monsoon rainfall[R]. College Station, TX: International Ocean Discovery Program, 2016.

    Google Scholar

    [24] France-Lanord C, Schwenk T, Klaus A. Expedition 354 scientific prospectus: Bengal fan[R]. International Ocean Discovery Program, 2014.

    Google Scholar

    [25] France-Lanord C, Spiess V, Klaus A. Expedition 354 preliminary report: Bengal fan[R]. International Ocean Discovery Program, 2015.

    Google Scholar

    [26] France-Lanord C, Spiess V, Klaus A, et al. Proceedings of the international ocean discovery program 354: Bengal Fan[R]. College Station, 2016.

    Google Scholar

    [27] Sarin M M, Krishnaswami S, Dilli K, et al. Major ion chemistry of the Ganga-Brahmaputra river system: Weathering processes and fluxes to the Bay of Bengal [J]. Geochimica et Cosmochimica Acta, 1989, 53(5): 997-1009. doi: 10.1016/0016-7037(89)90205-6

    CrossRef Google Scholar

    [28] Phillips S C, Johnson J E, Underwood M B, et al. Long-timescale variation in bulk and clay mineral composition of Indian continental margin sediments in the Bay of Bengal, Arabian Sea, and Andaman Sea [J]. Marine and Petroleum Geology, 2014, 58: 117-138. doi: 10.1016/j.marpetgeo.2014.06.018

    CrossRef Google Scholar

    [29] Venkatarathnam K, Biscay P E. Clay mineralogy and sedimentation in the eastern Indian Ocean [J]. Deep Sea Research and Oceanographic Abstracts, 1973, 20(8): 729-738.

    Google Scholar

    [30] Pattan J N, Shane P, Banakar V K. New occurrence of Youngest Toba Tuff in abyssal sediments of the Central Indian Basin [J]. Marine Geology, 1999, 155(3-4): 243-248. doi: 10.1016/S0025-3227(98)00160-1

    CrossRef Google Scholar

    [31] Weber M E, Wiedicke-Hombach M, Kudrass H R, et al. Bengal Fan sediment transport activity and response to climate forcing inferred from sediment physical properties [J]. Sedimentary Geology, 2003, 155(3-4): 361-381. doi: 10.1016/S0037-0738(02)00187-2

    CrossRef Google Scholar

    [32] Tripathy G R, Singh S K, Ramaswamy V. Major and trace element geochemistry of Bay of Bengal sediments: Implications to provenances and their controlling factors [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 397: 20-30. doi: 10.1016/j.palaeo.2013.04.012

    CrossRef Google Scholar

    [33] Ramaswamy V, Kumar B V, Parthiban G, et al. Lithogenic fluxes in the Bay of Bengal measured by sediment traps [J]. Deep Sea Research Part I:Oceanographic Research Papers, 1997, 44(5): 793-810. doi: 10.1016/S0967-0637(96)00117-3

    CrossRef Google Scholar

    [34] Colin C, Turpin L, Bertaux J, et al. Erosional history of the Himalayan and Burman ranges during the last two glacial–interglacial cycles [J]. Earth and Planetary Science Letters, 1999, 171(4): 647-660. doi: 10.1016/S0012-821X(99)00184-3

    CrossRef Google Scholar

    [35] Kessarkar P M, Rao V P, Ahmad S M, et al. Changing sedimentary environment during the Late Quaternary: Sedimentological and isotopic evidence from the distal Bengal Fan [J]. Deep Sea Research Part I:Oceanographic Research Papers, 2005, 52(9): 1591-1615. doi: 10.1016/j.dsr.2005.01.009

    CrossRef Google Scholar

    [36] Chang Z H, Zhou L P. Evidence for provenance change in deep sea sediments of the Bengal Fan: A 7 million year record from IODP U1444A [J]. Journal of Asian Earth Sciences, 2019, 186: 104008. doi: 10.1016/j.jseaes.2019.104008

    CrossRef Google Scholar

    [37] Li J R, Liu S F, Shi X F, et al. Clay minerals and Sr-Nd isotopic composition of the Bay of Bengal sediments: implications for sediment provenance and climate control since 40 ka [J]. Quaternary International, 2018, 493: 50-58. doi: 10.1016/j.quaint.2018.06.044

    CrossRef Google Scholar

    [38] Xue P F, Chang L, Wang S S, et al. Magnetic mineral tracing of sediment provenance in the central Bengal Fan [J]. Marine Geology, 2019, 415: 105955. doi: 10.1016/j.margeo.2019.05.014

    CrossRef Google Scholar

    [39] 方念乔, 陈学方, 胡超涌, 等. 东北印度洋深海记录基本特征及其对青藏高原隆升的响应[J]. 第四纪研究, 2001, 21(6):490-499 doi: 10.3321/j.issn:1001-7410.2001.06.004

    CrossRef Google Scholar

    FANG Nianqiao, CHEN Xuefang, HU Chaoyong, et al. Deep sea sedimentary records in the Northeastern Indian Ocean and their response to the uplift of the Qinghai-Xizang Plateau [J]. Quaternary Sciences, 2001, 21(6): 490-499. doi: 10.3321/j.issn:1001-7410.2001.06.004

    CrossRef Google Scholar

    [40] 方念乔, 陈萍, 吴琳, 等. 孟加拉湾深海记录中的等深流活动特征及其环境意义初探[J]. 地球科学—中国地质大学学报, 2002, 27(5):570-575

    Google Scholar

    FANG Nianqiao, CHEN Ping, WU Lin, et al. Contour currents in deep-water records from Bay of Bengal and its environmental implication [J]. Earth Science-Journal of China University of Geosciences, 2002, 27(5): 570-575.

    Google Scholar

    [41] Lee J, Kim S, Lee J I, et al. Monsoon-influenced variation of clay mineral compositions and detrital Nd-Sr isotopes in the western Andaman Sea (IODP Site U1447) since the late Miocene [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 538: 109339. doi: 10.1016/j.palaeo.2019.109339

    CrossRef Google Scholar

    [42] Bergmann F, Schwenk T, Spiess V, et al. Middle to late Pleistocene architecture and stratigraphy of the lower Bengal fan—integrating multichannel seismic data and IODP expedition 354 results [J]. Geochemistry, Geophysics, Geosystems, 2020, 21(1): e2019GC008702.

    Google Scholar

    [43] Weber M E, Reilly B T. Hemipelagic and turbiditic deposits constrain lower Bengal Fan depositional history through Pleistocene climate, monsoon, and sea level transitions [J]. Quaternary Science Reviews, 2018, 199: 159-173. doi: 10.1016/j.quascirev.2018.09.027

    CrossRef Google Scholar

    [44] Xie P P, Arkin P A. Global precipitation: a 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputs [J]. Bulletin of the American Meteorological Society, 1997, 78(11): 2539-2558. doi: 10.1175/1520-0477(1997)078<2539:GPAYMA>2.0.CO;2

    CrossRef Google Scholar

    [45] Li J R, Liu S F, Shi X F, et al. Sedimentary responses to the sea level and Indian summer monsoon changes in the central Bay of Bengal since 40 ka [J]. Marine Geology, 2019, 415: 105947. doi: 10.1016/j.margeo.2019.05.006

    CrossRef Google Scholar

    [46] 李吉均. 青藏高原的地貌演化与亚洲季风[J]. 海洋地质与第四纪地质, 1999, 19(1):1-11 doi: 10.16562/j.cnki.0256-1492.1999.01.002

    CrossRef Google Scholar

    LI Jijun. Studies on the geomorphological evolution of the Qinghai-Xizang (Tibetan) Plateau and Asian Monsoon [J]. Marine Geology & Quaternary Geology, 1999, 19(1): 1-11. doi: 10.16562/j.cnki.0256-1492.1999.01.002

    CrossRef Google Scholar

    [47] Raymo M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate [J]. Nature, 1992, 359(6391): 117-122. doi: 10.1038/359117a0

    CrossRef Google Scholar

    [48] Wang G C, Cao K, Zhang K X, et al. Spatio-temporal framework of tectonic uplift stages of the Tibetan Plateau in Cenozoic [J]. Science China Earth Sciences, 2011, 54(1): 29-44. doi: 10.1007/s11430-010-4110-0

    CrossRef Google Scholar

    [49] 张克信, 王国灿, 洪汉烈, 等. 青藏高原新生代隆升研究现状[J]. 地质通报, 2013, 32(1):1-18 doi: 10.3969/j.issn.1671-2552.2013.01.001

    CrossRef Google Scholar

    ZHANG Kexin, WANG Guocan, HONG Hanlie, et al. The study of the Cenozoic uplift in the Tibetan Plateau: a review [J]. Geological Bulletin of China, 2013, 32(1): 1-18. doi: 10.3969/j.issn.1671-2552.2013.01.001

    CrossRef Google Scholar

    [50] Tada R, Zheng H B, Clift P D. Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau [J]. Progress in Earth and Planetary Science, 2016, 3(1): 4. doi: 10.1186/s40645-016-0080-y

    CrossRef Google Scholar

    [51] Prell W L, Kutzbach J E. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution [J]. Nature, 1992, 360(6405): 647-652. doi: 10.1038/360647a0

    CrossRef Google Scholar

    [52] Burbank D W, Derry L A, France-Lanord C. Reduced Himalayan sediment production 8 Myr ago despite an intensified monsoon [J]. Nature, 1993, 364(6432): 48-50. doi: 10.1038/364048a0

    CrossRef Google Scholar

    [53] An Z S, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan Plateau since Late Miocene times [J]. Nature, 2001, 411(6833): 62-66. doi: 10.1038/35075035

    CrossRef Google Scholar

    [54] Clemens S, Prell W, Murray D, et al. Forcing mechanisms of the Indian Ocean monsoon [J]. Nature, 1991, 353(6346): 720-725. doi: 10.1038/353720a0

    CrossRef Google Scholar

    [55] Weber M E, Lantzsch H, Dekens P, et al. 200, 000 years of monsoonal history recorded on the lower Bengal Fan - strong response to insolation forcing [J]. Global and Planetary Change, 2018, 166: 107-119. doi: 10.1016/j.gloplacha.2018.04.003

    CrossRef Google Scholar

    [56] 方念乔, 丁旋, 陈学方, 等. 孟加拉湾MD77190柱状样第3期的韵律沉积记录及快速气候变化[J]. 第四纪研究, 1999(6):511-517 doi: 10.3321/j.issn:1001-7410.1999.06.003

    CrossRef Google Scholar

    FANG Nianqiao, DING Xuan, CHEN Xuefang, et al. Rapid climatic change in oxygen isotope stage 3: evidence from the rhythmic sedimentary record in core MD77190, Bengal Bay [J]. Quaternary Sciences, 1999(6): 511-517. doi: 10.3321/j.issn:1001-7410.1999.06.003

    CrossRef Google Scholar

    [57] 方念乔, 陈学方, 丁旋, 等. 孟加拉湾和东经90°海岭260ka以来的古海洋学记录与印度季风的影响[J]. 中国科学(D辑), 2001, 31(S1):280-286

    Google Scholar

    FANG Nianqiao, CHEN Xuefang, DING Xuan, et al. Paleoceanogrphic records of Bengal Bay and Ninety East Ridge since the last 260 ka and its response to Indian Monsoon [J]. Science in China (Series D), 2001, 31(S1): 280-286.

    Google Scholar

    [58] Contreras-Rosales L A, Jennerjahn T, Tharammal T, et al. Evolution of the Indian summer monsoon and terrestrial vegetation in the Bengal region during the past 18 ka [J]. Quaternary Science Reviews, 2014, 102: 133-148. doi: 10.1016/j.quascirev.2014.08.010

    CrossRef Google Scholar

    [59] Gaina C, Müller R D, Brown B, et al. Breakup and early seafloor spreading between India and Antarctica [J]. Geophysical Journal International, 2007, 170(1): 151-169. doi: 10.1111/j.1365-246X.2007.03450.x

    CrossRef Google Scholar

    [60] Desa M A, Ramana M V. Middle Cretaceous geomagnetic field anomalies in the Eastern Indian Ocean and their implication to the tectonic evolution of the Bay of Bengal [J]. Marine Geology, 2016, 382: 111-121. doi: 10.1016/j.margeo.2016.10.002

    CrossRef Google Scholar

    [61] Yatheesh V, Dyment J, Bhattacharya G C, et al. Detailed structure and plate reconstructions of the Central Indian Ocean between 83.0 and 42.5 Ma (Chrons 34 and 20) [J]. Journal of Geophysical Research:Solid Earth, 2019, 124(5): 4305-4322. doi: 10.1029/2018JB016812

    CrossRef Google Scholar

    [62] 尚鲁宁, 胡刚, 袁忠鹏, 等. 东北印度洋85°E海脊的性质和起源: 综述和新认识[J]. 海洋地质与第四纪地质, 2020, 40(4):1-16

    Google Scholar

    SHANG Luning, HU Gang, YUAN Zhongpeng, et al. Tectonic structure and origin of the 85°E ridge, Northeastern Indian Ocean: A review and new observations [J]. Marine Geology & Quaternary Geology, 2020, 40(4): 1-16.

    Google Scholar

    [63] Mishra D C. Magnetic crust in the Bay of Bengal [J]. Marine Geology, 1991, 99(1-2): 257-261. doi: 10.1016/0025-3227(91)90095-L

    CrossRef Google Scholar

    [64] Mukhopadhyay M, Krishna M B R. Gravity anomalies and deep structure of the Ninetyeast Ridge north of the equator, eastern Indian Ocean- a hot spot trace model [J]. Marine Geophysical Researches, 1995, 17(2): 201-216. doi: 10.1007/BF01203426

    CrossRef Google Scholar

    [65] Curray J R, Munasinghe T. Origin of the Rajmahal Traps and the 85°E Ridge: preliminary reconstructions of the trace of the Crozet hotspot [J]. Geology, 1991, 19(12): 1237-1240. doi: 10.1130/0091-7613(1991)019<1237:OOTRTA>2.3.CO;2

    CrossRef Google Scholar

    [66] Müller R D, Royer J Y, Lawver L A. Revised plate motions relative to the hotspots from combined Atlantic and Indian Ocean hotspot tracks [J]. Geology, 1993, 21(3): 275-278. doi: 10.1130/0091-7613(1993)021<0275:RPMRTT>2.3.CO;2

    CrossRef Google Scholar

    [67] Kent R W, Storey M, Saunders A D, et al. Comment and reply on “origin of the Rajmahal traps and the 85°E ridge: preliminary reconstructions of the trace of the Crozet hotspot” [J]. Geology, 1992, 20(10): 957-959. doi: 10.1130/0091-7613(1992)020<0957:CAROOO>2.3.CO;2

    CrossRef Google Scholar

    [68] Ramana M V, Subrahmanyam V, Chaubey A K, et al. Structure and origin of the 85°E Ridge [J]. Journal of Geophysical Research:Solid Earth, 1997, 102(B8): 17995-18012. doi: 10.1029/97JB00624

    CrossRef Google Scholar

    [69] Ismaiel M, Krishna K S, Srinivas K, et al. Internal structure of the 85°E ridge, Bay of Bengal: Evidence for multiphase volcanism [J]. Marine and Petroleum Geology, 2017, 80: 254-264. doi: 10.1016/j.marpetgeo.2016.11.020

    CrossRef Google Scholar

    [70] Anand S P, Rajaram M, Majumdar T J, et al. Structure and tectonics of 85°E Ridge from analysis of Geopotential data [J]. Tectonophysics, 2009, 478(1-2): 100-110. doi: 10.1016/j.tecto.2008.09.036

    CrossRef Google Scholar

    [71] Shang L N, Hu G, Pan J, et al. Hotspot volcanism along a leaky fracture zone contributes the formation of the 85°E Ridge at 11°N latitude, Bay of Bengal [J]. Tectonophysics, 2022, 837: 229453. doi: 10.1016/j.tecto.2022.229453

    CrossRef Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(8)

Tables(1)

Export Citation
PDF
XML

Article Metrics

Article views(1491) PDF downloads(30) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020