刘康^1,2,3,,
郝天珧^1,2,3,,,
杨辉⁴,
文百红⁴,
贺恩远⁵
1. 中国科学院地质与地球物理研究所, 中国科学院油气资源研究重点实验室, 北京 100029
2. 中国科学院地球科学研究院, 北京 100029
3. 中国科学院大学, 北京 100049
4. 中国石油勘探开发研究院, 北京 100083
5. 中国科学院南海海洋研究所, 中国科学院边缘海地质重点实验室, 广州 510301

基金项目: 地质调查海洋地质保障工程项目（GZH200900504-207），国家自然科学基金面上基金（41476033），国家自然科学基金联合基金（U1505232），"全球变化与海气相互作用"专项国际合作项目（GASI-GEOGE-01）、国家重点研发计划"超深层重磁电震勘探技术研究"项目（2016YFC0601102，2016YFC0601104）和国家科技重大专项"下古生界-前寒武系碳酸盐岩油气成藏规律、关键技术及目标评价"（2016ZX05004003）共同资助


详细信息

作者简介: 刘康, 男, 1989年生, 中国科学院地质与地球物理研究所博士研究生毕业.现为同济大学国家海底科学观测系统项目办公室专业技术人员, 主要从事地震仪器研发、面波勘探和综合地球物理研究工作.E-mail:liukang@mail.iggcas.ac.cn

通讯作者: 郝天珧, 女, 1957年生, 中国科学院地质与地球物理研究所研究员, 主要从事海陆油气盆地综合地球物理研究.E-mail:tyhao@mail.iggcas.ac.cn

中图分类号: P223;P631

收稿日期:2018-01-07
修回日期:2018-07-17
上线日期:2018-10-05

Model analysis combining gravity and seismic data with the response of inhomogeneous mantle

LIU Kang^1,2,3,,
HAO TianYao^1,2,3,,,
YANG Hui⁴,
WEN BaiHong⁴,
HE EnYuan⁵
1. Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2. Institutes of Earth Science, Chinese Academy of Sciences, Beijing 100029, China
3. University of Chinese Academy of Sciences, Beijing 100049, China
4. Research Institute of Petroleum Exploration and Development, Beijing 100083, China
5. Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China


More Information

Corresponding author: HAO TianYao,E-mail:tyhao@mail.iggcas.ac.cn

MSC: P223;P631

--> Received Date: 07 January 2018
Revised Date: 17 July 2018
Available Online: 05 October 2018


摘要
摘要:本文提出在综合地球物理研究中，为了使重力数据处理和反演更加符合实际的地质情况，重力-地震联合建模分析时应当考虑非均匀地幔物质的重力效应.本文针对含油气盆地结构、断裂构造、大陆边缘演化和洋陆转换带等热点地质问题，广泛调研了全球范围内多个地区的综合地球物理研究成果，及其对应的地幔深部结构，发现地幔的横向不均一性是普遍存在的.在以往许多基于重力、地震数据的综合研究实践中，重力异常分离和建模分析通常都是在地壳内部（莫霍面以上）进行的.这种处理方式实际上是以均匀地幔为假设前提，虽然简化了重力异常分离和建模分析的难度，但忽略了地球深部的不均匀性所带来的重力异常，所获得的剩余重力异常和在此基础上进行的密度结构反演、地质解释会存在偏差.本文通过对模型界面的2D正演，定量探讨了非均匀地幔对布格重力异常的影响.在对四川盆地的实例研究中，剥离了非均匀地幔的重力效应，2.5D重震联合模拟的结果明显优于均匀地幔假设条件下的结果.
关键词: 综合地球物理/
非均匀地幔/
2.5维建模分析/
重力异常分离/
地震/
四川盆地

Abstract:This paper proposes a new strategy for conducting model analysis with gravity anomaly and seismic data, in which the gravity response of inhomogeneous mantle should be taken into account. Model calculations and a case study in the Sichuan basin demonstrate this strategy a good potential to make the gravity data processing and inversion more consistent with the actual geological conditions. By collecting the comprehensive geophysical research results in many regions around the world, as well as the corresponding deep mantle structure, we find the lateral inhomogeneity of the mantle is widely distributed in the petroliferous basins, continental margins, ocean-continent transitions and other geological sites of general interest. However, in many joint studies based on gravity and seismic data, model analysis is usually performed within the crust. Although it simplifies the difficulty of the model analysis, the gravity anomaly caused by deep earth inhomogeneity should have been considered, otherwise the inverted density structure and interpretations may deviate the actual geological conditions. Therefore, based on the 2D forward modeling, this paper evaluates the quantitative effect of inhomogeneous mantle on Bouguer anomaly. Moreover, in a case study of the Sichuan basin, the results of the 2.5D joint simulation taking into account the inhomogeneous mantle are obviously better than those of following the homogeneous mantle hypothesis.
Key words:Integrated geophysics/
Inhomogeneous mantle/
2.5D model analysis/
Gravity anomaly separation/
Seismic data/
Sichuan basin



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