石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (2): 285-298.doi: 10.11743/ogg20210203
陈槚俊1,2(), 何登发1,2, 孙方源1, 田方磊1,2
收稿日期:
2020-05-18
出版日期:
2021-04-28
发布日期:
2021-04-21
作者简介:
陈槚俊(1993—),男,博士研究生,矿产普查与勘探。E-mail: 基金资助:
Jiajun Chen1,2(), Dengfa He1,2, Fangyuan Sun1, Fanglei Tian1,2
Received:
2020-05-18
Online:
2021-04-28
Published:
2021-04-21
摘要:
塔北隆起奥陶系大型油气田的发现促进了地质学家对该地区早古生代构造格局的探讨。早古生代不整合的地理、几何和时间变量解析有助于认识塔北古隆起的形成过程。基于大量的钻井和地震资料,解析了塔北隆起地区志留系底、顶部不整合,厘定了古隆起在晚奥陶世末和中泥盆世末的形态和展布范围,最终探讨了古构造应力场的演变。研究表明,塔北隆起地区志留系底、顶部不整合面都具有“下削上超”不整合结构,即不整合面之下的地层被削截,而年轻地层超覆于不整合面之上。隆起范围在晚奥陶世末期近东西向展布,而中泥盆世末期在南部斜坡上转变为3个古凸起(英买力低凸起、轮南低凸起、库尔勒鼻状凸起),整体上呈北东-南西向展布。晚奥陶世末近东西向的古隆起在中泥盆世末叠加了北东-南西向的构造,表明挤压应力场由晚奥陶世的南北向逐渐转变为北西-南东向。为已取得的关于塔北晚加里东期古隆起格局的认识提供了重要科学依据,并给予了详细的论证。
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