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岩浆岩侵入煤层范围的地震解释方法

崔大尉 邨于景 戴方尧

煤田地质与勘探Issue(2):76-79,4.
煤田地质与勘探Issue(2):76-79,4.DOI:10.3969/j.issn.1001-1986.2014.02.016

岩浆岩侵入煤层范围的地震解释方法

Seismic interpretation method for the magmatic intrusion extent in coal seams

崔大尉 1邨于景 2戴方尧3

作者信息

  • 1. 煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221008
  • 2. 中国矿业大学资源与地球科学学院,江苏 徐州 221116
  • 3. 中国矿业大学资源与地球科学学院,江苏 徐州 221116
  • 折叠

摘要

Abstract

The magmatic intrusion in the coal seams brings about a great effect on coal safe production, so it is very important to locate the boundary of the magmatic intrusion in coal. In this paper, the seismic interpretation method for the magmatic intrusion in the coal is put forward, including three kinds of lithology interpretation methods, i.e. seismic inversion, seismic face analysis and spectrum decomposition. The property of the method is to utilize comprehensively drilling data and seismic dynamic information of high impedance, high frequency and waveform difference. The practical 3D seismic data in a coal mine, Huaibei, Anhui Province are interpreted with the method, and reliable geological basis is supplied for the boundary of the magmatic intrusion in coal.

关键词

岩浆岩/三维地震/地震反演/地震相分析/谱分解

Key words

magmatic rocks/3D seismic/seismic inversion/seismic face analysis/spectrum decomposition

分类

天文与地球科学

引用本文复制引用

崔大尉,邨于景,戴方尧..岩浆岩侵入煤层范围的地震解释方法[J].煤田地质与勘探,2014,(2):76-79,4.

基金项目

国家自然科学基金与神华集团有限责任公司联合资助项目(U1261202) (U1261202)

煤田地质与勘探

OA北大核心CSCDCSTPCD

1001-1986

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