论文部分内容阅读
位于中国大陆西部的塔里木盆地是中国大陆面积最大(56×104km2)的含油气沉积盆地。塔里木陆块由前震旦变质基底和显生宙海-陆叠合沉积盆地组成,其东、西两端分别与“北中国陆块”与“卡拉库姆陆块”相邻,其南、北两侧分别为特提斯体系的“帕米尔—西昆仑—阿尔金弧形山系”和古亚洲体系的“天山—北山弧形山系”所包围。将“塔里木陆块及其周缘造山系”作为研究“陆块”与“两大体系”之间对接的典型地域,是最
The Tarim Basin, located in western China, is the largest oil-bearing basin in mainland China (56 × 104 km 2). The Tarim block consists of the former Sinian metamorphic basement and the Phanerozoic marine-continental superimposed sedimentary basin. The east and west ends of the Tarim block are adjacent to the “northern China land block” and the “Karakum block, respectively” Its south and north sides are respectively surrounded by the “Pamir-West Kunlun-Argun arc-shaped mountain system” of the Tethys system and the “Tianshan-Beishan arc-shaped mountain system” of the ancient Asian system. The typical area where the “Tarim block and its peripheral orogenic system” is used as the docking area between the research on “land block” and “two systems” is the most