塔里木盆地巴楚隆起区构造-热演化历史研究  

A study on tectono-thermal evolution history of Bachu uplift in Tarim basin

作　　者：于靖波[1] 张健[1] 史保平[1] 

机构地区：[1]中国科学院研究生院计算地球动力学重点实验室,北京100049

出　　处：《地球物理学报》2010年第10期2396-2404,共9页Chinese Journal of Geophysics

基　　金：国家重点基础研究"973"课题(G2007CB411704;G2008CB425704);中国科学院知识创新工程重要方向项目(kzcx2-yw-203-01)资助

摘　　要：巴楚隆起是塔里木盆地重要勘探地区之一,其构造-热演化史制约着该区烃的生成、运移及聚集.本文在恢复巴楚地区4条地震解释剖面沉积埋藏史的基础上,通过求解热传导方程,计算了它们的构造-热演化历史.计算过程中首先利用"回剥"法,确定莫霍面处的热流值,再利用地壳重力均衡原理,求得各时期的莫霍面埋深,最终确定盆地基底热流和地表热流.结果表明,该地区构造-热演化可以划分为7个阶段,其中三叠纪热演化阶段地温梯度及地表热流达到最高值,分别为32℃/km和73.6 mW/m^2,而现今地温梯度及地表热流值最低,分别为20℃/km和46.4 mW/m^2.计算得出的现今地表热流密度值略大于实测值,分析认为主要由于中新世以来,巴楚隆起区侧向热扩散加快了地表热流的衰减所致.最后在模拟基础上,探讨了生热率、热导率对盆地热演化的影响.Bachu uplift is one of the major oil prospect areas in Tarim basin. Its tectono-thermal evolution significantly influence hydrocarbons formation, migration and accumulation. In this paper, we reveal the burial histories of four seismic profiles spanning Bachu uplift and present the tectono-thermal history of this region by solving two-dimensional heat conduction equation. During the simulation, we calculate the average heat flow value at Moho surface by using ＂back tripping＂ method. Then we employ the principle of isostatics to compute the burial depths of Moho surface during geological period, finally we calculate the basal and surface heat flow of the basin. The numerical results show that the tectono-thermal history of this region can be divided into seven stages. The maximum of the geothermal gradient and heat flow appeared in Triassic period with the value of 32℃/kin and 73. 6 mW/m2 respectively, and the minimum of them appears now, the values are 20℃/kin and 46.4 mW/m2 respectively. Because of lateral thermal diffusion since the Miocene Epoch, the average heat flow value of the calculation is slightly greater than actual value. At last, we discuss the influence of thermal conductivity and heat generation on thermal evolution of a basin.

关 键 词：塔里木盆地 构造-热演化 数值模拟 热流密度 

分 类 号：P314[天文地球—固体地球物理学]