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塔里木盆地显生宙的沉积历史始于早震旦世,深入研究其含油气性时,有十大风格引人瞩目:(1)静海盆地相和举足轻重的加里东运动;(2)从沙漠—海湾相、古亚洲定局到华力西最后一次碰撞事件;(3)两类三个三叠纪盆地;(4)中—新生代两个前陆盆地共拥一个中央隆起;(5)背冲推覆和前陆滑脱是两类基本构造样式;(6)典型的前陆盆地及明显的前渊迁移有序性;(7)普遍存在不整合与削截圈闭;(8)晚期成藏和“大气晚成”;(9)南天山和铁克里克隆起下面都有影子盆地;(10)四个并存和多源多期成藏。
The sedimentary history of the Phanerozoic in the Tarim Basin began in the Early Sinian. When studying its oil and gas content in depth, it attracted the attention of ten major styles: (1) the pivotal Caledonian movement in the Jinghai Basin; and (2) Gulf phase, the last collision of ancient Asia to Varys; (3) two types of three Triassic basins; (4) mid-Cenozoic two foreland basins hold a central uplift; Nappe and foreland slippage are two basic structural styles; (6) the orderly migration of typical foreland basins and distinct forelands; (7) unconformities and cut-off traps; (8) late accumulation And “late blooms”; (9) there are shadow basins beneath the uplifted South Tianshan and Iron Creek; and (10) four coexisting and multi-source multi-phase reservoirs.