论南海新生代的构造运动
On tectonic movement in the South China Sea during the Cenozoic
-
摘要: 白垩纪末和新生代之交的构造运动揭开了新生代南海多旋回构造运动的序幕,自此之后整个南海的地壳开始进入总体受张性背景区域构造应力场控制、以张性沉降为主要特征的地质发展时期.七次区域性的构造运动和沉积作用具有多旋回、周期性振荡式发生的特点,其中尤以白垩纪末和老第三纪初、晚始新世和中渐新世及中中新世和晚中新世之间的三次构造运动表现最为强烈,形成了南海最为重要的三个区域性构造界面.南海地壳运动是欧亚、太平洋和印度—澳大利亚三大板块相互作用效应的结果和缩影,是跨越太平洋和印度—澳大利亚两大板块更大范围的岩石圈和软流圈流动(运动)方向、速度和强度的周期性振荡式改变所导致的.Abstract: The tectonic movement at the end of Cretacious and the beginning of Cenozoic had opened the Cenozoic phase of poly cyclic tectonic movement,then the whole crust of the South China Sea had been mainly subjected to the regional stress field of tectonic tension,which was characterized by rifting depression.Seven times of regional tectonic movement and sedimentation had been assembled into ageological development history of polycyclic oscillatory.Especially,the tectonic movement was strongly intensified at the end of Cretacious and the beginning of Paleagene,between the Late Eocene and the Mid-Oligocene, during the Mid-and Late Miocene.These three times of tectonic movement had built the most important regional tectonic interfaces in the South China Sea.Crust movement of the South China Sea was the result and epitome of interaction of the Eurasia,Pacific and Indo)Australia plates,that is,they were introduced by polycyclic changes of directions,rates and strengths of lithospheric movement and asthenospheric flow covering across the Pacific and Indo)Australia plates.
-
Key words:
- South China Sea /
- Cenozoic /
- tectonic movement
-
KARIG D E.Origin and development of marginal basin in the western Pacific[J].Geophys Res,1971,76:2 542-2 561. KARIG D E.Plate convergence between the Philippines and Ryukyu Islands[J].Mar Geology,1973,14:153-168. BEN-AVRAHAM Z,UYEDA S.The evolution of the China Basin and Mesozoic paleogeography of Borneo[J].Earth and Planet Sci Lett,1973,18:365-376. TAYLOR B,HAYES D E.The tectonic evolution of the South China Sea Basin.HAYES D E.The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands.Geophys Monogr:Vol.23[M].Washington D C:AGU,1980.89-104. TAYLOR B,HAYES D E.Origin and history of the South China Sea Basin.HAYES D E.The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands:Part 2.Geophys Monogr:Vol.27[M].Washington D C:AGU,1983.23-56. 李振五.南海中部北部地壳结构的探讨[J].地球物理学报,1984,27(2):153-165. 何廉声,姚伯初.南海北部大陆边缘上的声纳浮标测量(二)——陆缘地壳结构构造[J].海洋地质与第四纪地质,1983,3(4):57-68. 何廉声.大地构造说明书.南海地质地球物理图集[Z].广州:广东地图出版社,1987. 何廉声.多旋回的板块构造与南海新生代构造[J].南海地质研究,1988,98-108. 姚伯初,王光宇.南海海盆的地壳结构[J].中国科学(B辑),1983,2:177-186. 姚伯初.南海海盆在新生代的构造演化[J].南海地质研究,1991,(3):9-23. 姚伯初.南海北部陆缘新生代构造初探[J].南海地质研究,1993,(5):1-12. 姚伯初,曾维军,HAYES D E,等.中美合作调研南海地质专报[R].武汉:中国地质大学出版社,1994. 姚伯初,万玲,刘振湖,等.南海南部海域新生代万安运动的构造意义及其油气资源效应[J].海洋地质与第四纪地质,2004,24(1):69-77. 陈邦彦.地壳结构图.南海地质地球物理图集[Z].广州:广东地图出版社,1987. 陈邦彦.地壳结构图说明书.南海地质地球物理图集[Z].广州:广东地图出版社,1987. 吕文正.南海中央海盆条带磁异常特征及构造演化[J].海洋学报,1987,9(1):69-78. 金翔龙.南海地球科学研究报告[J].东海海洋,1989,7(4):1-92. 李德生,杜永林.中国沿海大陆架新生代含油气盆地的地质特征[J].海洋学报,1983,5(6):766-776. 李德生,姜仁旗.南海东沙隆起及其周围坳陷的地质演化[J].海洋学报,1989,11(6):737-741. 金庆焕.南海地质与油气资源[M].北京:地质出版社,1989. 金庆焕,李唐根.南沙海域区域地质构造[J].海洋地质与第四纪地质,2000,20(1):1-8. 任继舜,陈廷愚,牛宝贵,等.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京:科学出版社,1990. 刘光鼎.中国海区及邻域地质地球物理特征[M].北京:科学出版社,1992. 陈国达.亚洲陆海壳体大地构造[M].长沙:湖南教育出版社,1998. 吴能友,曾维军,宋海斌,等.南海区域构造沉降特征[J].海洋地质与第四纪地质,2003,23(1):55-64. 陈圣源.南海磁异常特征[A].刘光鼎.中国海区及邻域地质地球物理特征[M].北京:科学出版社,1992. 刘金萍,阎贫,赵明辉.南海西南海盆地震反射特征及其形成时代[J].海洋地质与第四纪地质,2003,23(1):67-71. 林长松,虞夏军,何拥华,等.南海海盆扩张成因质疑[J].海洋学报,2006,28(1):67-76. 林长松,高金耀,虞夏军,等.南海北部新生代的构造运动特征[J].海洋学报,2006,28(4):81-86. 刘海玲,阎贫,张伯友,等.南海前新生代基底与东特提斯构造域[J].海洋地质与第四纪地质,2004,24(1):15-28. 郑家坚,何希贤,刘淑文,等.中国地层典:第三系[M].北京:地质出版社,1999. 曾维军.广州-巴拉望地学断面[A].刘光鼎.中国海区及邻域地质地球物理特征[M].北京:科学出版社,1992.272-288. HINZ K,SCHLUTER.Geology of the dangerous grounds,South China Sea,and the continental margin off southwest Palawan:results of SONNE cruises S0-23 and S0-27[J].Energy,1985,10(3-4):297-315. 钟志洪,王良书,李绪宣,等.琼东南盆地古近纪沉积充填演化及其区域构造意义[J].海洋地质与第四纪地质,2004,24(1):29-36 张文佑,李荫槐,刘昭蜀,等.中国及邻区海陆大地构造[M].北京:科学出版社,1986. 吴进民.南海西部地震层序的时代分析[J].南海地质研究,1994,(6):16-29. МАТВЕЕНКОВВВ,СЕДОВАП.пeрцодичнocтьвнутриплитнoгo вуЛканизмай[J].Океанология,1996,36(4):606-611. JACKSON E D,SHAW H R,BAGGAR K E.Calculated geochronology and stress field orientation along the Hawiian chain[J].Earth and Planet Sci Lett,1975,26:145-155. HILDE T W C,UYEDA S,KROENKE L.Evolution of the Western Pacific and its margin[J].Tectonophysics,1977,38(1-2):145-165. LEE T Y,LAWVER L A.Cenozoic plate reconstruction of Southeast Asia[J].Tectonophysics,1995,251(1-4):85-138. 赵政璋,李永铁,叶和飞,等.青藏高原大地构造特征及盆地演化[M].北京:科学出版社,2001.
点击查看大图
计量
- 文章访问数: 792
- HTML全文浏览量: 6
- PDF下载量: 1385
- 被引次数: 0