论菲律宾海板块大地构造分区

吴时国; 范建柯; 董冬冬

doi:10.3969/j.issn.0563-5020.2013.03.008

论菲律宾海板块大地构造分区

- 1.
  中国科学院海洋研究所, 中国科学院海洋地质与环境重点实验室青岛 266071
- 2. 中国科学院研究生院北京 100049

详细信息

作者简介:
吴时国, 男, 1963年9月生, 研究员, 海洋地球物理学与构造地质学专业。E-mail:swu@qdio.ac.cn

中图分类号: P542

收稿日期: 2012-06-10

修回日期: 2012-12-12

刊出日期: 2013-07-25

Discussion on the tectonic division of the Philippine Sea Plate

- 1.
  Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071
- 2. Graduate University of Chinese Academy of Sciences, Beijing 100049

Received Date: 10 June 2012

Revised Date: 12 December 2012

Publish Date: 25 July 2013

摘要

摘要: 菲律宾海板块是毗邻中国大陆的一个独特的小型板块。除南端表现十分复杂外,它的构造边界多以海沟为界,比较清楚,然而次级大地构造单元划分则比较复杂。本文根据近年来的研究成果,按照块体构造理论注重统一的地球物理场、相似的地壳结构、有机的成因联系等3个基本原则,将菲律宾海板块划分为3个具有不同构造演化特征的单元,即西菲律宾海块体、四国—帕里西维拉块体和伊豆—博宁—马里亚纳块体。西菲律宾海块体包括两部分:一个是西菲律宾海盆,始新世以来受太平洋板块和印澳板块近南北向的相对俯冲作用影响,并顺时针旋转形成了现今的构造样式,于30 Ma左右停止扩张。另一个包括大东盆岭、花东盆地、帕劳海盆和吕宋岛弧蛇绿岩等洋壳在内的白垩纪洋盆。根据形成年代和形成时的扩张方向可将四国—帕里西维拉块体分为两部分:四国海盆和帕里西维拉海盆,两者以索夫干断裂为界。伊豆—博宁—马里亚纳块体沿博宁高原南缘分为南北两部分,两者表现出不同的地质特征。
- 菲律宾海 /
- 板块 /
- 块体 /
- 大地构造
Abstract: Philippine Sea Plate(PSP)is a unique minor plate close to China mainland.Except for the complicated southern part, the tectonic boundaries of the PSP are clear, most of which consist of trenches.However, it is hard to divide the plate into the secondary even three-level units.Based on the research in the recent years and referring to block tectonic theory with the principals of unitary geophysical field, similar crustal structure and organic genesis, the PSP is partitioned into three units with different evolutionary history, i.e.West Philippine Sea Block(WPSB), Shikoku-Parece Vela Block(SPB)and Izu-Bonin-Mariana Block(IBMB).The WPSB consists of two major parts, Cenozoic oceanic basin(west Philippine Basin)which was opened between two opposed subduction zones, rotated clockwise to the present place and culminated at ca.30 Ma, and Cretaceous oceanic basin consisting of Daito Basin and ridge province, Huatung Basin, Palau Basin and ophiolite of Luzon arc.The SPB can be divided further into Shikoku Basin and Parece Vela Basin by the Sofugan Fault.The IBMB displays the different geological features in the south and north of the Bonin(Ogasawara)Plateau.
- Philippine Sea /
- Plate /
- Block /
- Tectonics

HTML全文

参考文献(59)

[1]	刘光鼎.1992.中国海区及邻域地质地球物理场特征.北京:科学出版社.1—424.
[2]	Liu Guangding.1992.Features of Geophysical Fieldsand Geodynamics of China Seas and Adjacent Areas.Beijing:Science Press.1—424.
[3]	刘光鼎.2007.中国大陆构造格架的动力学演化.地学前缘, 14 (3): 39—46.
[4]	Liu Guangding.2007.Geodynamical evolution and tectonic framework of China.Earth Science Frontiers, 14 (3): 39—46.
[5]	吴时国,喻普之.2006.海底构造学导论.北京:科学出版社.1—306.
[6]	Wu Shiguo and Yu Puzhi.2006.Introduction on Seafloor Tectonics.Beijing:Science Press.1—306.
[7]	张训华,孟祥君,韩波.2009.块体与块体构造学说.海洋地质与第四纪地质, 29 (5): 59—64.
[8]	Zhang Xunhua,Meng Xiangjun and Han Bo.2009.Block and block tectonics.Marine Geology & Quaternary Geology, 29 (5): 59—64.
[9]	Cande S and Kent D V.1995.Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic.Journal of Geophysical Research, 100 (B4): 6093—6095.
[10]	Chamot-Rooke N,Renard V and LePichon X.1987.Magnetic anomalies in the Shikoku Basin:A new interpretation. Earth and Planetary Science Letters, 83 (1—4): 214—228.
[11]	Cosca M A,Arculus R J,Pearce J A et al.1998. ⁴⁰Ar/³⁹Ar and K-Ar geochronological age constraints for the inception and early evolution of the Izu-Bonin-Mariana arc system,Island Arc, 7 (3): 579—595.
[12]	Defant M J,Jacques D,Maury R C et al.1989.Geochemistry and tectonic setting of the Luzon arc,Philippines.Geological Society of America Bulletin, 101 (5): 663—672.
[13]	Deschamps A,Lallemand S and Collot J Y.1998.A detailed study of the Gagua ridge: A fracture zone uplifted during a plate reorganization in the Mid-Eocene.Marine Geophysical Researches, 20: 403—423.
[14]	Deschamps A,Monie P,Lallemand S et al.2000.Evidence for Early Cretaceous oceanic crust trapped in the Philippine Sea Plate.Earth Planetary Science Letters, 179 (3—4): 503—516.
[15]	Deschamps A and Lallemand S.2002.The west Philippine Basin:An Eocene to early Oligocene back arc basin opened between two opposed subduction zones.Journal of Geophysical Research, 107 (B12):doi:10.1029/2001JB001706.
[16]	Dimalanta C B and Yumul G P.2006.Magmatic and amagmatic contributions to crustal growth in the Philippine island arc system:Comparison of the Cretaceous and post-Cretaceous periods.Geosciences Journal, 10 (3): 321—329.
[17]	Fujioka K,Okino K,Kanamatsu T et al.1999.Enigmatic extinct spreading center in the west Philippine backarc basin unveiled.Geology, 27 (12): 1135—1138.
[18]	Fujiwara T,Tamaki K,Fujimoto H et al.1995.Morphological studies of the Ayu Trough,Philippine Sea-Caroline Plate boundary.Geophysical Research Letters, 22 (2): 109—112.
[19]	Hall C E,Gurnis M,Sdrolias M et al.2003.Catastrophic initiation of subduction following forced convergence across fracture zones.Earth and Planetary Science Letters, 212 (1—2): 15—30.
[20]	Hall R.1987.Plate boundary evolution in the Halmahera region:Indonesia.Tectonophysics, 144 (4): 337—352.
[21]	Hall R,Ali J R,Anderson C D et al.1995.Origin and motion history of the Philippine Sea Plate.Tectonophysics, 251 (1—4): 229—250.
[22]	Hickey-Vargas R.1998.Origin of the Indian Ocean-type isotopic signature in basalts from Philippine Sea Plate spreading centers:An assessment of local versus large-scale processes.Journal of Geophysical Research, 103 (B9): 20963—20979.
[23]	Hickey-Vargas R.2005.Basalt and tonalite from the Amami Plateau,northern west Philippine Basin:New Early Cretaceous ages and geochemical results,and their petrologic and tectonic implications.Island Arc, 14 (4): 653—665.
[24]	Hickey-Vargas R,Bizimis M and Deschamps A.2008.Onset of the Indian Ocean istopic signature in the Philippine Sea Plate:Hf and Pb isotope evidence from Early Cretaceous terranes.Earth Planetary Science Letters, 268 (3—4): 255—267.
[25]	Hilde T W C and Lee C S.1984.Origin and evolution of the west Philippine Basin:A new interpretation.Tectonophysics, 102 (1—4): 85—104.
[26]	Kao H M,Lee C S,Hsu S K and Wang C.1999.Magnetic ages in the east and south of Taiwan offshore areas and its possible tectonic evolution,abstract in SEASIA Conference,May 9～12th,Montpellier,France.277—279.
[27]	Karig D E.1975.Basin Genesis in the Philippine Sea.In:Initial Reports of the Deep Sea Drilling Project,Vol.31.857—879.
[28]	Kasuga S and Ohara Y.1997.A new model of back～arc spreading in the Parece Vela Basin.northwest Pacific margin.Island Arc, 6 (3): 316—326.
[29]	Kearey P,Klepeis K A and Vine F J.2009.Global Tectonics, 3^rd Edition.Wiley-Blackwell.1—482.
[30]	Lee C S,Hsu S K,Okino K et al.1999.Deep Drag Ocean Bottom Magnetometer and Its Application on the Tertiary Magnetic Isochrons.Abstract in Geophysical Meeting,Keelung,October 28—29th.
[31]	Louden K E.1976.Magnetic anomalies in the west Philippine Basin.Geophysical Monograph Series, 19: 253—267.
[32]	Malyarenko A N and Lelikov E P.1995.Granites and associated rocks in the Philippine Sea and the East China Sea.In:Tokuyama H,Shcheka S A,Isezaki N et al.(Eds.).Geology and Geophysics of the Philippine Sea.Terrapub,Tokyo.311—328.
[33]	Matsuda J.1985.Sr isotope studies of rocks from Philippine Sea and some implication for the mantle material.In:Shiki T(Ed.).Geology of the Northern Philippine Sea.Tokai:Tokai University Press.63—78.
[34]	McIntosh K D and Nakamura Y.1998.Crustal structure beneath the Nanao forearc basin from TAICRUST MCS/OBS line 14.TAO, 9 (3): 345—362.
[35]	McKee E H.1974.K-Ar ages of deep-sea basalts,Benham rise,west Philippine Basin. In: Initial Reports of the Deep Sea Drilling Project,Leg 31.599—600.
[36]	McKee E H and Klock P R.1980.K-Ar ages of basalts sills from Deep Sea Drilling Project Sites 444 and 446,Shikoku Basin and Daito Basin,Philippine Sea.Deep Sea Drilling Project Reports and Publications, 58: 921—922.
[37]	Mitchell J G,Peate D W,Murton B J et al.1992.K-Ar dating of basement rocks from the Izu-Bonin outer-arc high,ODP Leg 125.In:Fryer P,Pearce J A,Stokking L B et al.(Eds.).Proceedings of the Ocean Drilling Program,Scientific Results,Vol.125,Ocean Drilling Program,College Station,TX.203—210.
[38]	Mrozowski C L and Hayes D E.1979.The evolution of the Parece Vela Basin,eastern Philippine Sea.Earth and Planetary Science Letters, 46 (1): 49—67.
[39]	Mrozowski C L,Lewis S D and Hayes D E.1982.Complexities in the tectonic evolution of the west Philippine Basin.Tectonophysics, 82 (1—2): 1—24.
[40]	Nichols G,Hall R,Milsom J et al.1990.The southern termination of the Philippine trench.Tectonophysics, 183 (1—4): 289—303.
[41]	Okino K,Shimakawa Y and Nagaoka S.1994.Evolution of the Shikoku Basin.Journal of Geomagnetism and Geoelectricity, 46 (6): 463—479.
[42]	Okino K,Kasuga S and Ohara Y.1998.A new scenario of the Parece Vela Basin genesis.Marine Geophysical Researches, 20 (1): 21—40.
[43]	Okino K,Ohara Y,Kasuga S et al.1999.The Philippine Sea:A new survey results reveal the structure and history of the marginal basins.Geophysical Research Letters, 26 (15): 2287—2290.
[44]	Okino K and Fujioka K.2003.The central basin spreading center,Philippine Sea:Structure of an extinct spreading center and implications for marginal basin formation.Journal of Geophysical Research, 108 (B1):doi:10.1029/2001JB001095.
[45]	Okino K,Ohara Y,Fujiwara T et al.2009.Tectonics of the southern tip of the Parece Vela Basin,Philippine Sea Plate.Tectonophysics, 466 (3—4): 213—228.
[46]	Ozima M,Takigami Y and Kaneoka Ⅰ.1980. ⁴⁰Ar/³⁹Ar geochronological studies on rocks of Deep-Sea Drilling Project sites 443, 445 and 446.Initial Reports of the Deep Sea Drilling Project,Leg 58.917—920.
[47]	Ozima M,Kaneoka Ⅰ,Saito K et al.1983.Summary of geochronological studies of submarine rocks from the western Pacific Ocean.Geodynamics Series, 11: 137—142.
[48]	Rangin C,Le Pichon X,Mazzotti S et al.1999.Plate convergence measured by GPS across the Sundaland/Philippine Sea Plate deformed boundary:The Philippines and eastern Indonesia.Geophysical Journal International, 139 (2): 296—316.
[49]	Ranken B,Cardwell R K and Karig D E.1984.Kinematics of the Philippine Sea Plate,Tectonics, 3 (5): 555—575.
[50]	Salisbury M H,Shinohara M,Richter C et al.2002.Proc.ODP,Init.Repts. , 195:College Station,TX(Ocean Drilling Program).doi:10.297 3/odp.proc.ir.195.2002.
[51]	Scott R B,Kroenke L W,Zakariadze G et al.1980.Evolution of the South Philippine Sea:Deep Sea Drilling Project Leg 59 Results.Washington:US Government Printing Office.803—815.
[52]	Sdrolias M,Roest W R and Müller R D.2004.An expression of Philippine Sea Plate rotation:The Parece Vela and Shikoku basins.Tectonophysics, 394 (1—2): 69—86.
[53]	Shiki T,Mizuno A and Kobayashi K.1985.Data listing of the bottom materials dredged and cored from the northern Philippine Sea.In:Shiki T(Ed.).Geology of the Northern Philippine Sea.Tokyo:Tokai University Press.23—41.
[54]	Sibuet J C,Hsu S K,Le Pichon X et al.1999.Philippine Sea Plate and Taiwan Sea Plates:Formation of Taiwan.Abstract in SEASIA Conference,May 9～12th,Montpellier,France.21.
[55]	Suyehiro K,Takahashi N,Ariie Y et al.1996.Continental crust,crustal underplating,and low-Q upper mantle beneath an oceanic island arc.Science, 272 (5260): 390—392.
[56]	Takahashi N,Kodaira S,Klemperer S L et al.2007.Crustal structure and evolution of the Mariana intra-oceanic island arc. Geology, 35 (3): 203—206.
[57]	Taylor B and Goodliffe A M.2004.The west Philippine Basin and the initiation of subduction,revisited.Geophysical Research Letters, 31 (12):L12602.
[58]	Tokuyama H.1995.Origin and development of the Philippine Sea.In:Tokuyama H,Sheheka N,Isezaki N et al.(Eds.).Geology and Geophysics of the Philippine Sea.Terra Science Publisher,Tokyo.155—163.
[59]	Yang Y S and Wang T K.1998.Crustal velocity variation of the western Philippine Sea Plate from TAICRUST OBS/MCS line 23.TAO, 9 (3): 379—393.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 6104
PDF下载数: 1932
施引文献: 0

论菲律宾海板块大地构造分区

作者简介: 吴时国, 男, 1963年9月生, 研究员, 海洋地球物理学与构造地质学专业。E-mail:swu@qdio.ac.cn

Discussion on the tectonic division of the Philippine Sea Plate

计量

出版历程

目录

作者简介:
吴时国, 男, 1963年9月生, 研究员, 海洋地球物理学与构造地质学专业。E-mail:swu@qdio.ac.cn