塔里木盆地古生代充填层序和沉积样式
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摘要
本文在研究大量地震反射剖面的基础上,结合钻井地质成果,进行地震层序划分和对比,将塔里木古生代盆地充填序列划分为震旦—奥陶系、志留—泥盆系和石炭—二叠系等3个超层序,进一步划分出9个层序,确定并讨论了每个层序的地质属性、地质时代、层序地层格架和沉积样式。
Based on seismic reflection data and drilling results, the Paleozoic basin-fill sequences can be divided into three super-sequences, i.e., Sinian to Ordovician, Silurian to Devonian and Permian to Carboniferous which include nine sequences. The geological contribution, time, sequence stratigraphic framework and sedimentary style of each sequence are also discussed in this paper.
Based on seismic reflection data and drilling results, the Paleozoic basin-fill sequences can be divided into three super-sequences, i.e., Sinian to Ordovician, Silurian to Devonian and Permian to Carboniferous which include nine sequences. The geological contribution, time, sequence stratigraphic framework and sedimentary style of each sequence are also discussed in this paper.
引文
① 樊太亮等,1994,新疆塔里木盆地北部层序地层学应用研究,“八五”国家科技攻关项目研究成果报告。
① 熊剑飞,李静琏等,1994,新疆塔里木盆地地层层序及区域对比研究,“八五”国家科技攻关项目研究成果报告。
[1] Allen P A and J, R. Allen. Basin analysis: principles and applications: Oxford, London. Biackwen Scientific Publications
[2] 刘和甫,梁慧社,蔡立国,夏义平,刘立群.天山两侧前陆冲断系构造样式与前陆盆地演化.地球科学.中国地质大学学报,1994,18(6) :699～724
[3] Sloss L L. Tectonic evolution of the craton in Phanerozoic time, in Sloss, L. L., ed., Seclimentary cover: North American craton, U. S. The Geology of North America, Volume D-2:25～51
[4] 姜春发,施希德,胡金庆等.昆仑开合构造.北京:地质出版社,1992
① 熊剑飞,李静琏等,1994,新疆塔里木盆地地层层序及区域对比研究,“八五”国家科技攻关项目研究成果报告。
[1] Allen P A and J, R. Allen. Basin analysis: principles and applications: Oxford, London. Biackwen Scientific Publications
[2] 刘和甫,梁慧社,蔡立国,夏义平,刘立群.天山两侧前陆冲断系构造样式与前陆盆地演化.地球科学.中国地质大学学报,1994,18(6) :699～724
[3] Sloss L L. Tectonic evolution of the craton in Phanerozoic time, in Sloss, L. L., ed., Seclimentary cover: North American craton, U. S. The Geology of North America, Volume D-2:25～51
[4] 姜春发,施希德,胡金庆等.昆仑开合构造.北京:地质出版社,1992
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