南海西南次海盆NH973-1测线地震解释
摘要
针对973项目"南海大陆边缘动力学与油气资源潜力"2009年新采集的多道地震剖面NH973 1测线进行了研究分析,获得以下初步认识:(1)西南次海盆深海平原南端下伏巨厚沉积体,表明陆坡坡脚不是洋陆边界的位置,深海平原南端为陆壳分布区,也可解释为洋陆过渡带.这种情况在南海的洋陆边界确定过程中应加以考虑.(2)西南次海盆洋壳基底存在两种类型,反映了不同海底扩张阶段岩浆活动与变形的强弱不同,与扩张速率变化有关.
We interpreted the new 2-D multi-channel seismic profile line NH973-1 which crossed southwest sub-basin of South China Sea(SCS)and was acquired in 2009 by Project-973 "South China Sea continental margin dynamics and petroleum resource potential".Our preliminary analyses are as follows:(1)We observed the thick sedimentary body beneath the abyssal plain at the southern end of southwestern sub-basin,considered that continental crust exists beneath the thick sedimentary body,and the toe of southern continental slope is not the COB(Continental and Oceanic crust Boundary),but is in COT(Continental and Oceanic crust Transition)zone. Therefore,it is necessary to consider this situation before we determine the COB of SCS.(2) There are two types of oceanic crust basement,which reflects different spreading rate, magmatism,and deformation for different stages of seafloor spreading.
We interpreted the new 2-D multi-channel seismic profile line NH973-1 which crossed southwest sub-basin of South China Sea(SCS)and was acquired in 2009 by Project-973 "South China Sea continental margin dynamics and petroleum resource potential".Our preliminary analyses are as follows:(1)We observed the thick sedimentary body beneath the abyssal plain at the southern end of southwestern sub-basin,considered that continental crust exists beneath the thick sedimentary body,and the toe of southern continental slope is not the COB(Continental and Oceanic crust Boundary),but is in COT(Continental and Oceanic crust Transition)zone. Therefore,it is necessary to consider this situation before we determine the COB of SCS.(2) There are two types of oceanic crust basement,which reflects different spreading rate, magmatism,and deformation for different stages of seafloor spreading.
引文
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[9]Hayes D E.The tectonic evolution of the Great South China Sea.AAPG Bull,1990,74:978
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[12]Tapponnier P,Peltzer G,Armijo R.On the mechanics of the collision between India and Asia.In:Coward M P,Ries A C,ed.Collision Tectonics.Geological Society,London, Special Publications,1986,19:115-157
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[14]Hall R.Cenozoic plate reconstructions of SE Asia.In:Hall R,Blundell D J,eds.Tectonic Evolution of Southeast Asia. Geological Society,London,SpecialPublications,1997,106: 153-184
[15]Longley I M.The tectonostratigraphic evolution of SE Asia. In:Murphy R W,ed.Petroleum Geology of Southeast Asia. Geological Society,London,Special Publications,1997, 126:311-339
[16]Murphy R W.SE Asia reconstruction with a non-rotation Cenozoic Borneo.Geological Society of Malaysia Bulletin, 1998,42:85-94
[17]Hall R.Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific:computer-based reconstructions, model andanimations.Journal of Asian Earth Sciences, 2002,20(4):353-431
[18]Hutchison C S,Bergman S C,Swauger D A,et al.A miocene collisional belt in north Borneo,uplift mechanism and isostatic adjustment quantified by thermochronology. Journal of the Geological Society,2000,157(4):783-793
[19]Fuller M,Ali JR,Moss S J,et al.Paleomagnetism of borneo.Journal of Asian Earth Sciences,1999,17(1-2): 3-24
[20]Searle M P.Role of the Red River Shear zone,Yunnan and Vietnam,in the continental extrusion of SE Asia.Journal of the Geological Society,2006,163(6):1025-1036
[21]Hall R,van Hattum M W A,Spakman W.Impact of India-Asia collision on SE Asia:the record in Borneo.Tectonophysics, 2008,451(1-4);366-389
[22]Cullen A,Reemst P,Henstral G,et al.Rifting of the South China Sea:new perspectives.Petroleum Geoscience,2010, 16(3):273-282
[23]张训华.单向拉张与南海海盆的形成.海洋地质动态,1 997, (5):1-3 Zhang X H.One-way extension and the formation of the South China Sea basin.Marine Geology Letters(in Chinese), 1997,(5):1-3
[24]姚伯初,万玲.南海岩石圈厚度变化特征及其构造意义.中国地质,2010,37(4):888-899 Yao B C,Wan L.Variation of the lithospheric thickness in theSouth China Sea area and its tectonic significance. Geology in China(in Chinese),2010,37(4):888-899
[25]李家彪,金翔龙,高金耀.南海东部海盆晚期扩张的构造地貌研究.中国科学(D辑),2002,32(3):239-248 Li J B,Jin X L,Gao J Y.Tectonic geomorphology research of the late expansion in the Eastern South China Sea.Sci. China(Series D)(in Chinese),2002,32(3):239~248
[26]丁巍伟,陈汉林,杨树锋等.南海西南次海盆与东部次海盆地质与地球物理分析.高校地质学报,2002,8(3):268- 279 Ding W W,Chen H L,Li S F,et al.Geological and geophysical analysis of the Southwestern and Eastern subbasins, South China Sea.Geological Journal of China Universities(in Chinese),2002,8(3):268-279
[27]丁巍伟,陈汉林,杨树锋等.南海深海盆磁异常分析及其动力学意义.浙江大学学报(理学版),2003,30(2):223-229 Ding W W,Chen H L,Li S F,et al.Apply the interpolation cut method in magnetic anomaly analyse of the South China Sea.Journal of Zhejiang University(Science Edition)(in Chinese),2003,30(2):223-229.
[28]张健,宋海斌,李家彪.南海西南海盆构造演化的热模拟研究.地球物理学报,2005,48(6):1357-1365 Zhang J,Song H B,Li J B.Thermal modeling of the tectonic evolution of the southwest subbasin in the South China Sea. Chinese J.Geophys.(in Chinese),2005,48(6):1357-1365
[29]孙珍,钟志洪,周蒂等.南海的发育机制研究:相似模拟证据.中国科学(D辑):地球科学,2006,36(9):797-810 Sun Z,Zhong Z H,Zhou D,et al.Mechanism of development oftheSouth ChinaSea:evidenceof similar simulation.Sci.China(Series D ):Earth Sciences.(in Chinese),2006,36(9):797-810
[30]孙珍,孙龙涛,周蒂等.南海岩石圈破裂方式与扩张过程的三维物理模拟.地球科学—中国地质大学学报,2009, 34(3):435-447 Sun Z,Sun L T,Zhou D,et al.Discussion on the South China Sea evolution and lithospheric breakup through 3D analogue modeling.Earth Science Journal of China University of Geosciences(in Chinese),2009,34(3):435-447
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