西太平洋洋底高原内部结构与形成演化

张锦昌; 罗怡鸣; 李海勇; 杨博; 黄彦铭

doi:10.3981/j.issn.1000-7857.2023.02.008

科技导报 >

2023 , Vol. 41 >Issue 2: 65 - 79

DOI: https://doi.org/10.3981/j.issn.1000-7857.2023.02.008

专题：太平洋火山研究前沿

西太平洋洋底高原内部结构与形成演化

张锦昌 ,
罗怡鸣 ,
李海勇 ,
杨博 ,
黄彦铭

展开

1. 中国科学院边缘海与大洋地质重点实验室, 中国科学院南海海洋研究所, 南海生态环境工程创新研究院, 广州 511458;
2. 南方海洋科学与工程广东省实验室 (广州), 广州 511458;
3. 中国-巴基斯坦地球科学研究中心, 中国科学院-巴基斯坦高等教育委员会, 巴基斯坦伊斯兰堡 45320;
4. 南方科技大学海洋科学与工程系, 深圳 518055;
5. 油气资源与勘探技术教育部重点实验室 (长江大学), 武汉 430100

张锦昌,研究员,研究方向为海洋地质与地球物理,电子信箱:jzhang@scsio.ac.cn

收稿日期: 2022-10-20

修回日期: 2022-12-22

网络出版日期: 2023-02-10

基金资助

南方海洋科学与工程广东省实验室（广州）人才团队引进重大专项（GML2019ZD0205）；广东省基础与应用基础研究基金项目（2021B1515020098，2019A1515011244）；国家自然科学基金项目（41890813，41976066，42006056，91958212）；中国科学院项目（133244KYSB20180029，131551KYSB20200021，Y4SL021，QYZDY-SSW-DQC005，ISEE2021PY03）；广东省重点领域研发计划项目（2020B1111520001）；中国博士后科学基金资助项目（2022M711480）

收起

Structure and formation of oceanic plateaus in west Pacific Ocean

ZHANG Jinchang ,
LUO Yiming ,
LI Haiyong ,
YANG Bo ,
HUANG Yanming

Expand

1. CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 511458, China;
2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China;
3. China-Pakistan Joint Research Center on Earth Science, CAS-HEC, Islamabad 45320, Pakistan;
4. Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China;
5. Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Wuhan 430100, China

Received date: 2022-10-20

Revised date: 2022-12-22

Online published: 2023-02-10

Fold

摘要

洋底高原是在深海盆地中最显著的大火成岩省，记录着海洋大规模的岩浆活动，对研究地壳结构、板块构造、地幔动力学乃至地球演化历史都具有重要意义。西太平洋是洋底高原分布最密集的区域，是研究洋底高原内部结构与形成演化的最佳场所。选取西太平洋中最具代表性的6座洋底高原——沙茨基海隆、赫斯海隆、麦哲伦海隆、翁通爪哇高原、马尼希基高原以及希古朗基高原，通过对这6座洋底高原地质概况的简要描述，归纳近年来获得的地球物理与地球化学重要观测结果，揭示其内部结构的共性，包括大面积地形隆起、异常厚的地壳、异常负的地幔重力异常以及形成于洋中脊之上或者附近的位置特征；探索了其形成机制，即地幔柱与洋中脊的相互作用可能是洋底高原的主要成因。

关键词： 大火成岩省; 洋底高原; 地幔柱; 洋中脊; 西太平洋

本文引用格式

张锦昌 , 罗怡鸣 , 李海勇 , 杨博 , 黄彦铭 . 西太平洋洋底高原内部结构与形成演化[J]. 科技导报, 2023 , 41(2) : 65 -79 . DOI: 10.3981/j.issn.1000-7857.2023.02.008

Abstract

Oceanic plateaus are the most remarkable large igneous provinces in deep sea basins. They document massive magmatism in the oceans, and are important for better understanding crustal structure, plate tectonics, mantle geodynamics and Earth's evolution history. Oceanic plateaus are most developed in west Pacific Ocean, providing the optimal place to study their internal structure and formation. This paper selects six representative oceanic plateaus within west Pacific Ocean:Shatsky Rise, Hess Rise, Magellan Rise, Ontong Java Plateau, Manihiki Plateau and Hikurangi Plateau. We present brief geologic overview of each plateau and summarize major geophysical and geochemical observations. Based on the common characteristics of these plateaus, including massive topographic uplift, abnormally thick crust, negative mantle gravity anomaly, and formation on or near the mid-ocean ridge; the formation mechanisms are discussed, and the future investigations are suggested, i. e., interaction between mantle plume and mid-ocean ridge may be the main origin of oceanic plateaus.

Key words： large igneous province; oceanic plateau; mantle plume; mid-ocean ridge; west Pacific Ocean

参考文献

[1] Coffin M F, Eldholm O.Large igneous provinces:Crustal structure, dimensions, and external consequences[J].Reviews of Geophysics, 1994, 32(1):1-36.
[2] Macdougall J D.Continental flood basalts[M].Dordrecht:Springer Science & Business Media, 1988.
[3] Mahoney J J, Coffin M F.Large igneous provinces:Continental, oceanic, and planetary flood volcanism[M].Washington D C:American Geophysical Union, 1997.
[4] 张国伟, 李三忠.西太平洋-北印度洋及其洋陆过渡带:古今演变与论争[J].海洋地质与第四纪地质, 2017, 37(4):1-17.
[5] Morgan W J.Deep mantle convection plumes and plate motions[J].AAPG bulletin, 1972, 56(2):203-213.
[6] Richards M A, Duncan R A, Courtillot V E.Flood basalts and hot-spot tracks:Plume heads and tails[J].Science, 1989, 246(4926):103-107.
[7] Anderson D L, Tanimoto T, Zhang Y.Plate tectonics and hotspots:The third dimension[J].Science, 1992, 256(5064):1645-1651.
[8] Foulger G R.The "plate" model for the genesis of melting anomalies[M]//Plates, Plumes and Planetary Processes.Boulder:Geological Society of America, 2007, 430:1.
[9] Rogers G C.Oceanic plateaus as meteorite impact signatures[J].Nature, 1982, 299(5881):341-342.
[10] Ingle S, Coffin M F.Impact origin for the greater ontong java plateau[J].Earth and Planetary Science Letters, 2004, 218(1/2):123-134.
[11] Harris P T, Macmillan-Lawler M, Rupp J, et al.Geomorphology of the oceans[J].Marine Geology, 2014, 352:4-24.
[12] Sandwell D T, Müller R D, Smith W H, et al.New global marine gravity model from cryosat-2 and jason-1 reveals buried tectonic structure[J].Science, 2014, 346(6205):65-67.
[13] Müller R D, Sdrolias M, Gaina C, et al.Age, spreading rates, and spreading asymmetry of the world's ocean crust[J].Geochemistry, Geophysics, Geosystems, 2008, 9(4).
[14] 罗怡鸣, 张锦昌, 林间.太平洋大塔穆火山研究进展及对巨型洋底火山成因的启示[J].地球物理学进展, 2019, 34(2):781-795.
[15] Kuo B-Y, Forsyth D W.Gravity anomalies of the ridgetransform system in the South Atlantic between 31 and 34.5 s:Upwelling centers and variations in crustal thickness[J].Marine Geophysical Researches, 1988, 10(3):205-232.
[16] Canales J P, Ito G, Detrick R S, et al.Crustal thickness along the western galápagos spreading center and the compensation of the galápagos hotspot swell[J].Earth and Planetary Science Letters, 2002, 203(1):311-327.
[17] Parker R L.The rapid calculation of potential anomalies[J].Geophysical Journal International, 1973, 31(4):447-455.
[18] Nakanishi M, Sager W W, Klaus A.Magnetic lineations within shatsky rise, Northwest Pacific Ocean:Implications for hot spot-triple junction interaction and oceanic plateau formation[J].Journal of Geophysical Research:Solid Earth, 1999, 104(B4):7539-7556.
[19] Nakanishi M, Sager W W, Korenaga J.Reorganization of the pacific-izanagi-farallon triple junction in the late jurassic:Tectonic events before the formation of the shatsky rise[J].The Origin, Evolution, and Environmental Evolution of Oceanic Large Igneous Provinces:Geological Society of America Special Papers, 2015, 511:85-101.
[20] Huang Y, Sager W W, Zhang J, et al.Magnetic anomaly map of shatsky rise and its implications for oceanic plateau formation[J].Journal of Geophysical Research:Solid Earth, 2021, 126(2):e2019JB019116.
[21] Larson R L.Late jurassic and early cretaceous evolution of the western central Pacific Ocean[J].Journal of GeoMagnetism and Geoelectricity, 1976, 28(3):219-236.
[22] Tamaki K, Joshima M, Larson R L.Remanent early cretaceous spreading center in the central Pacific Basin[J].Journal of Geophysical Research:Solid Earth, 1979, 84(B9):4501-4510.
[23] Tamaki K, Larson R L.The mesozoic tectonic history of the magellan microplate in the western central pacific[J].Journal of Geophysical Research:Solid Earth, 1988, 93(B4):2857-2874.
[24] Nakanishi M, Tamaki K, Kobayashi K.Magnetic anomaly lineations from late jurassic to early cretaceous in the west-central Pacific Ocean[J].Geophysical Journal International, 1992, 109(3):701-719.
[25] Zhang J, Sager W W, Korenaga J.The seismic moho structure of shatsky rise oceanic plateau, Northwest Pacific Ocean[J].Earth and Planetary Science Letters, 2016, 441:143-154.
[26] Sager W W, Zhang J, Korenaga J, et al.An immense shield volcano within the shatsky rise oceanic plateau, Northwest Pacific Ocean[J].Nature Geoscience, 2013, 6(11):976-981.
[27] Huang Y, Sager W W, Tominaga M, et al.Magnetic anomaly map of ori massif and its implications for oceanic plateau formation[J].Earth and Planetary Science Letters, 2018, 501:46-55.
[28] Sager W W, Huang Y, Tominaga M, et al.Oceanic plateau formation by seafloor spreading implied by tamu massif magnetic anomalies[J].Nature Geoscience, 2019, 12(8):661-666.
[29] Mahoney J J, Duncan R A, Tejada M L G, et al.Jurassic-cretaceous boundary age and mid-ocean-ridge-type mantle source for shatsky rise[J].Geology, 2005, 33(3):185-188.
[30] Sano T, Shimizu K, Ishikawa A, et al.Variety and origin of magmas on shatsky rise, northwest pacific ocean[J].Geochemistry, Geophysics, Geosystems, 2012, 13(8).
[31] Heydolph K, Murphy D T, Geldmacher J, et al.Plume versus plate origin for the shatsky rise oceanic plateau (NW pacific):Insights from Nd, Pb and Hf isotopes[J].Lithos, 2014, 200:49-63.
[32] Sager W W, Sano T, Geldmacher J.Formation and evolution of shatsky rise oceanic plateau:Insights from iodp expedition 324 and recent geophysical cruises[J].EarthScience Reviews, 2016, 159:306-336.
[33] Verzhbitskii E V, Lobkovskii L I, Kononov M V, et al.Genesis of shatsky and hess oceanic rises in the Pacific ocean as deduced from geologic-geophysical data and numerical modeling[J].Geotectonics, 2006, 40(3):236-245.
[34] Fletcher M, Wyman D A, Zahirovic S.Mantle plumes, triple junctions and transforms:A reinterpretation of pacific cretaceous-tertiary lips and the laramide connection[J].Geoscience Frontiers, 2020, 11(4):1133-1144.
[35] Tejada M L G, Geldmacher J, Hauff F, et al.Geochemistry and age of shatsky, hess, and ojin rise seamounts:Implications for a connection between the shatsky and hess rises[J].Geochimica et Cosmochimica Acta, 2016, 185:302-327.
[36] Hilde T W, Isezaki N, Wageman J M.Mesozoic seafloor spreading in the North Pacific[J].The Geophysics of the Pacific Ocean Basin and its Margin, 1976, 19:205-226.
[37] Mammerickx J, Sharman G F.Tectonic evolution of the north pacific during the cretaceous quiet period[J].Journal of Geophysical Research:Solid Earth, 1988, 93(B4):3009-3024.
[38] Rea D K, Dixon J M.Late cretaceous and paleogene tectonic evolution of the north pacific ocean[J].Earth and Planetary Science Letters, 1983, 65(1):145-166.
[39] Pringle M S, Dalrymple G B.Geochronological constraints on a possible hot spot origin for hess rise and the wentworth seamount chain[M].Washington DC:American Geophysical Union, 1993:263-277.
[40] Vallier T L, Windom K E, Seifert K E, et al.Volcanic rocks cored on hess rise, western pacific ocean[J].Nature, 1980, 286(5768):48-50.
[41] Seifert K E, Vallier T L, Windom K E, et al.Geochemistry and petrology of igneous rocks, deep sea drilling project leg 62[M].Washington:U.S.Government Printing Office, 1981:945-953.
[42] Keating B H, Fryer P, Batiza R, et al.Seamounts, islands, and atolls[J].Washington DC:American Geophysical Union, 1987:43.
[43] Clouard V, Bonneville A.How many Pacific hotspots are fed by deep-mantle plumes[J].Geology, 2001, 29(8):695-698.
[44] Utsunomiya A, Suzuki N, Ota T.Preserved paleo-oceanic plateaus in accretionary complexes:Implications for the contributions of the pacific superplume to global environmental change[J].Gondwana Research, 2008, 14(1/2):115-125.
[45] Eldholm O, Coffin M F.Large igneous provinces and plate tectonics[J].Geophysical Monograph-American Geophysical Union, 2000, 121:309-326.
[46] Zakharov Y D, Pletnev S P, Mel'nikov M E, et al.The first finds of cretaceous belemnites from the magellan rise, Pacific Ocean[J].Russian Journal of Pacific Geology, 2007, 1(1):29-41.
[47] Kerr A C.Oceanic plateaus[M]//Treatise on Geochemistry.2nd ed.Amsterdam:Elsevier, 2014:631-667.
[48] Neal C R, Mahoney J J, Kroenke L W, et al.The ontong java plateau[J].Geophysical Monograph-American Geophysical Union, 1997, 100:183-216.
[49] Ridley V A, Richards M A.Deep crustal structure beneath large igneous provinces and the petrologic evolution of flood basalts[J].Geochemistry, Geophysics, Geosystems, 2010, 11(9):Q09006.
[50] Korenaga J.Why did not the ontong java plateau form subaerially[J].Earth and Planetary Science Letters, 2005, 234(3/4):385-399.
[51] Mahoney J J, Storey M, Duncan R A, et al.Geochemistry and geochronology of leg 130 basement lavas:Nature and origin of the ontong java plateau[C]//Proceedings of the Ocean Drilling Program, Scientific Results.College Station, TX Texas A & M University, 1993:3-22.
[52] Taylor B.The single largest oceanic plateau:Ontong java-manihiki-hikurangi[J].Earth and Planetary Science Letters, 2006, 241(3/4):372-380.
[53] Fitton J G, Mahoney J J, Wallace P J, et al.Origin and evolution of the Ontong Java Plateau[C]//Proceedings of the Ocean Drilling Program, Scientific Results.Geological Society of London, 2004:1-18.
[54] Fitton J G, Mahoney J J, Wallace P J, et al.Origin and evolution of the Ontong Java Plateau:Introduction[J].Geological Society, London, Special Publications, 2004, 229:151-158.
[55] Tejada M L G, Mahoney J J, Castillo P R, et al.Pinpricking the elephant:Evidence on the origin of the Ontong Java plateau from Pb-Sr-Hf-Nd isotopic characteristics of odp leg 192 basalts[J].Geological Society, London, Special Publications, 2004, 229(1):133-150.
[56] Herzberg C.Partial melting below the Ontong Java Plateau[J].Geological Society, London, Special Publications, 2004, 229(1):179-183.
[57] Chazey III W J, Neal C R.Large igneous province magma petrogenesis from source to surface:Platinum-group element evidence from Ontong Java Plateau basalts recovered during odp legs 130 and 192[J].Geological Society, London, Special Publications, 2004, 229(1):219-238.
[58] Pietsch R, Uenzelmann-Neben G.Paleocene pacific plate reorganization mirrored in formation of the suvarov trough, manihiki plateau[J].Journal of Geophysical Research:Solid Earth, 2016, 121(10):7013-7023.
[59] Ito G, Clift P D.Subsidence and growth of pacific cretaceous plateaus[J].Earth and Planetary Science Letters, 1998, 161(1/2/3/4):85-100.
[60] Hochmuth K, Gohl K, Uenzelmann-Neben G, et al.Multiphase magmatic and tectonic evolution of a large igneous province-evidence from the crustal structure of the Manihiki Plateau, Western Pacific[J].Tectonophysics, 2019, 750:434-457.
[61] Hussong D M, Wipperman L K, Kroenke L W.The crustal structure of the Ontong Java and manihiki oceanic plateaus[J].Journal of Geophysical Research:Solid Earth, 1979, 84(B11):6003-6010.
[62] Ingle S, Mahoney J J, Sato H, et al.Depleted mantle wedge and sediment fingerprint in unusual basalts from the manihiki plateau, central Pacific Ocean[J].Geology, 2007, 35(7):595-598.
[63] Hoernle K, Hauff F, Van Den Bogaard P, et al.Age and geochemistry of volcanic rocks from the hikurangi and manihiki oceanic plateaus[J].Geochimica et Cosmochimica Acta, 2010, 74(24):7196-7219.
[64] Timm C, Hoernle K, Werner R, et al.Age and geochemistry of the oceanic Manihiki Plateau, SW pacific:New evidence for a plume origin[J].Earth and Planetary Science Letters, 2011, 304(1/2):135-146.
[65] Golowin R, Portnyagin M, Hoernle K, et al.Geochemistry of deep Manihiki Plateau crust:Implications for compositional diversity of large igneous provinces in the western Pacific and their genetic link[J].Chemical Geology, 2018, 493:553-566.
[66] Davy B, Hoernle K, Werner R.Hikurangi plateau:Crustal structure, rifted formation, and gondwana subduction history[J].Geochemistry, Geophysics, Geosystems, 2008, 9(7):Q07004.
[67] Bradshaw J D.Cretaceous geotectonic patterns in the New Zealand region[J].Tectonics, 1989, 8(4):803-820.
[68] Davy B W.The influence of subducting plate buoyancy on subduction of the Hikurangi-chatham Plateau beneath the north island, New Zealand[J].Geology and Geophysics of Continental Margins, 1992, 53(53):75-92.
[69] Wood R, Davy B.The Hikurangi Plateau[J].Marine Geology, 1994, 118(1/2):153-173.
[70] Mortimer N, Parkinson D.Hikurangi plateau:A cretaceous large igneous province in the southwest Pacific ocean[J].Journal of Geophysical Research:Solid Earth, 1996, 101(B1):687-696.
[71] Ito G, Lin J, Gable C W.Dynamics of mantle flow and melting at a ridge-centered hotspot:Iceland and the mid-atlantic ridge[J].Earth and Planetary Science Letters, 1996, 144(1/2):53-74.
[72] Zhang H, Meng W, Zhao F.Study on the exploitation, utilization and cooperation of geothermal energy between Iceland and China[C]//IOP Conference Series:Earth and Environmental Science.Bristol:IOP Publishing, 2020:012010.
[73] Cannat M, Briais A, Deplus C, et al.Mid-atlantic ridgeazores hotspot interactions:Along-axis migration of a hotspot-derived event of enhanced magmatism 10 to 4 Ma ago[J].Earth and Planetary Science Letters, 1999, 173(3):257-269.
[74] Escartin J, Cannat M, Pouliquen G, et al.Crustal thickness of V-shaped ridges south of the azores:Interaction of the mid-atlantic ridge (36°-39° N) and the azores hot spot[J].Journal of Geophysical Research:Solid Earth, 2001, 106(B10):21719-21735.
[75] Ito G T, Lin J.Mantle temperature anomalies along the past and paleoaxes of the galápagos spreading center as inferred from gravity analyses[J].Journal of Geophysical Research:Solid Earth, 1995, 100(B3):3733-3745.
[76] Ito G, Lin J.Oceanic spreading center-hotspot interactions:Constraints from along-isochron bathymetric and gravity anomalies[J].Geology, 1995, 23(7):657-660.
[77] Georgen J E, Lin J, Dick H J.Evidence from gravity anomalies for interactions of the marion and bouvet hotspots with the southwest Indian ridge:Effects of transform offsets[J].Earth and Planetary Science Letters, 2001, 187(3/4):283-300.
[78] Zhang T, Lin J, Gao J Y.Interactions between hotspots and the southwest Indian ridge during the last 90 Ma:Implications on the formation of oceanic plateaus and intra-plate seamounts[J].Science China Earth Sciences, 2011, 54(8):1177-1188.
[79] Georgen J E, Kurz M D, Dick H J, et al.Low ³He/⁴He ratios in basalt glasses from the western southwest Indian ridge (10°-24° E)[J].Earth and Planetary Science Letters, 2003, 206(3/4):509-528.
[80] Janin M, Hémond C, Maia M, et al.The Amsterdam-St.Paul Plateau:A complex hot spot/dupal-flavored morb interaction[J/OL].Geochemistry, Geophysics, Geosystems, 2012, 13(9), https://doi.org/10.1029/2012GC004165.
[81] Cande S C, LaBrecque J L, Haxby W F.Plate kinematics of the south Atlantic:Chron C³⁴ to present[J].Journal of Geophysical Research:Solid Earth, 1988, 93(B11):13479-13492.
[82] Sager W W, Foulger G R.What built shatsky rise, a mantle plume or ridge tectonics[J].Special Paper of Geological Society of America, 2005, 388:721.
[83] Ito G, Lin J, Graham D.Observational and theoretical studies of the dynamics of mantle plume-mid-ocean ridge interaction[J].Reviews of Geophysics, 2003, 41(4):1017.
[84] 鄢全树, 石学法.洋中脊与地幔柱热点相互作用研究进展[J].海洋地质与第四纪地质, 2006, 26(5):131-138.
[85] Sager W W, Pueringer M, Carvallo C, et al.Paleomagnetism of igneous rocks from the shatsky rise:Implications for paleolatitude and oceanic plateau volcanism[J].Special Paper of Geological Society of America, 2015, 511:147-171.
[86] Ryan M P.The physical nature of the icelandic magma transport system[M]//Magma Transport and Storage.New York:Wiley, 1990.
[87] Sigmundsson F.Iceland geodynamics:Crustal deformation and divergent plate tectonics[M].Springer Science & Business Media, 2006.
[88] Gente P, Dyment J, Maia M, et al.Interaction between the mid-atlantic ridge and the azores hot spot during the last 85 myr:Emplacement and rifting of the hot spot-derived plateaus[J].Geochemistry, Geophysics, Geosystems, 2003, 4(10):8514.
[89] Campbell I H, Griffiths R W.Implications of mantle plume structure for the evolution of flood basalts[J].Earth and Planetary Science Letters, 1990, 99(1/2):79-93.
[90] Campbell I H, Griffiths R W.The changing nature of mantle hotspots through time:Implications for the chemical evolution of the mantle[J].The Journal of Geology, 1992, 100(5):497-523.
[91] Foulger G R.Plumes, or plate tectonic processes[J].Astronomy & Geophysics, 2002, 43(6):6-19.
[92] Foulger G R, Natland J H, Anderson D L.Genesis of the iceland melt anomaly by plate tectonic processes[M/OL]//Plates, plumes and paradigms.Boulder:Geological Society of America, 2005.[2022-09-28].https://doi.org/10.1130/0-8137-2388-4.595.
[93] Anderson D L, Natland J H.Mantle updrafts and mechanisms of oceanic volcanism[J].Proceedings of the National Academy of Sciences, 2014, 111(41):4298-4304.
[94] 宋晓晓, 李春峰.西太平洋科学大洋钻探的地球动力学成果[J].热带海洋学报, 2016, 35(1):17-30.
[95] 陆鹿, 严立龙, 李秋环, 等.洋底高原及其对地球系统意义研究综述[J].岩石学报, 2016, 32(6):1851-1876.
[96] Zhang J, Sager W W, Korenaga J.The shatsky rise oceanic plateau structure from two-dimensional multichannel seismic reflection profiles and implications for oceanic plateau formation[M]//The Origin, Evolution, and Environmental Impact of Oceanic Large Igneous Provinces.Boulder:Geological Society of America, 2015:103-206.
[97] 吴婷婷, 李三忠, 庞洁红, 等.IODP324航次FMS成像测井资料处理及其在Shatsky海隆构造研究中的应用[J].地球科学进展, 2010(7):753-765.
[98] Li S Z, Suo Y H, Yu S, et al.Orientation of joints and arrangement of solid inclusions in fibrous veins in the Shatsky Rise, NW Pacific:Implications for crack-seal mechanisms and stress fields[J].Geological Journal, 2016, 51:562-578.
[99] Dordevic M, Georgen J.Dynamics of plume-triple junction interaction:Results from a series of three-dimensional numerical models and implications for the formation of oceanic plateaus[J].Journal of Geophysical Research:Solid Earth, 2016, 121(3):1316-1342.
[100] Bredow E, Steinberger B.Variable melt production rate of the kerguelen hotspot due to long-term plume-ridge interaction[J].Geophysical Research Letters, 2018, 45(1):126-136.
[101] Doucet S, Scoates J S, Weis D, et al.Constraining the components of the Kerguelen mantle plume:A Hf-PbSr-Nd isotopic study of picrites and high-mgo basalts from the Kerguelen Archipelago[J].Geochemistry, Geophysics, Geosystems, 2005, 6(4):Q04007.
[102] Mittelstaedt E, Ito G.Plume-ridge interaction, lithospheric stresses, and the origin of near-ridge volcanic lineaments[J].Geochemistry, Geophysics, Geosystems, 2005, 6(6):Q06002.
[103] 李三忠, 侯方辉, 吕海青, 等.洋中脊-地幔柱, 地幔柱-海沟与海沟-洋中脊相互作用[J].海洋地质动态, 2004, 20(11):1-5.
[104] Zhang J, Chen J.Geophysical implications for the formation of the tamu massif-the earth's largest single volcano-within the shatsky rise in the northwest pacific ocean[J].Science Bulletin, 2017, 62(1):69-80.
[105] 罗怡鸣, 张锦昌, 林间.全球三大洋底高原重力异常与地壳厚度特征及对比研究[J].热带海洋学报, 2020, 39(4):100-115.
[106] Georgen J E, Lin J.Three-dimensional passive flow and temperature structure beneath oceanic ridge-ridgeridge triple junctions[J].Earth and Planetary Science Letters, 2002, 204(1/2):115-132.

Options

文章导航

摘要

本文引用格式

Abstract

参考文献

联系我们

访问统计

模态框（Modal）标题

摘要

本文引用格式

Abstract

参考文献

联系我们

访问统计