重力场谱矩及其在塔里木盆地地壳结构成像中的应用研究

YANG Wen-Cai, SUN Yan-Yun, HOU Zun-Ze, YU Chang-Qing
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引用次数: 2

摘要

现代地球物理技术提供了大量的地球物理场数据,这些数据包含了丰富的地壳结构信息,可用于基于数学物理理论的地质填图。研究表明,区域重力数据的高阶谱矩包含几何等高线面的信息,可用于某些类型地质构造的选择、定位和分类。利用布格重力资料的二阶谱矩,可以计算出其统计不变量和脊状参数,从而表征地壳变形带的特征,可用于绘制变形带的区域分布。强或弱脊状参数区域之间的边界代表不同结构单元的边界。我们可以进一步计算统计不变量的二阶谱矩来计算边界参数,在增加一些增强后,可以用来跟踪和定位结构边界。本文给出了塔里木盆地中脊和边界参数的全部计算公式,以及地壳结构分析的试验结果。研究结果准确定位了塔里木盆地深部高、低密度带,为盆地油气勘探提供了重要的基础图像。
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A STUDY ON SPECTRAL MOMENTS OF GRAVITY FIELD WITH APPLICATION TO CRUSTAL STRUCTURE IMAGING OF TARIM BASIN

Modern geophysical techniques provide great amount data of geophysical field that contain rich information about crustal structures, which can be extracted for geo-mapping based on theory of mathematical physics. This paper shows that the high-order spectral moments of regional gravity data include information of geometrical contour surface, which can be used for selection, positioning and classification of some types of geological structures. By using second-order spectral moments of Bouguer gravity data, one can calculate their statistical unvaried quantities and the ridge-like parameter, which characterizes the crustal deformation belts and can be used for mapping regional distribution of the deformation belts. The boundaries between areas of strong or weak ridge-like parameters represent boundaries of different structural units. We can further compute the second-order spectral moments of the statistical unvaried quantities to calculate the boundary parameter, which may be used for tracing and positioning the structural boundaries after some enhancement are added. This paper gives all the formula for computing the ridge and the boundary parameters, and testing results on crustal structural analysis in Tarim basin, Northwest China. As the results, deep High- and Low-density belts within the Tarim basin are located precisely, providing important basic images for oil/gas exploration in the basin.

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