利用重磁对应分析法对负磁异常区内油页岩的推断
Estimation of Oil Shale in Negative Magnetic Anomaly Zone by Means of Gravity and Magnetic Correspondence Analysis
DOI: 10.12677/AG.2017.72021, PDF, HTML, XML, 下载: 1,492  浏览: 3,000  国家科技经费支持
作者: 孙鹏飞:河北工程大学,河北 邯郸;高铁:沈阳地质矿产研究所,辽宁 沈阳
关键词: 重力数据磁法数据重磁对应分析汉中地区Gravity Data Magnetic Data Gravity and Magnetic Correspondence Analysis Hanzhoung Area
摘要: 汉中地区的油页岩是陆相沉积的侏罗纪沉积岩,成分以石英砂岩、高岭土为主,具有油页岩普遍特征,相对密度中等,磁性弱,不适合重磁处理。但由于研究区的造山运动,被火成岩入侵,含有金属矿物带和褶皱带,油页岩层被其切割。因此,反其道而行,首先利用常规重磁处理手段,剔除金属矿脉和褶皱,圈出负磁异常区;其次,改造重力对应分析法,提出新相关系数R',把负磁异常区内的符合要求的R'断定为油页岩存在的区域。为油页岩的探测提供了一种新的探测方法。
Abstract: The Hanzhong area of oil shale is Jurassic sedimentary rocks of continental deposit, mainly quartz sandstone, kaolin component, with common features of oil shale, relative density moderate, weak magnetism, not suitable for gravity and magnetic. But as a result of the orogeny, igneous intrusion, containing metal mineral zone and fold belt, the oil shale is the cutting. Therefore, thinking conversely, firstly, we can use the conventional gravity and magnetic method to remove metal veins and folds, as well to demarcate the negative magnetic anomaly area. secondly, corresponding to the transformation of the gravity analysis method, a new correlation coefficient is proposed, And the matching R' in the negative magnetic anomaly region is determined as the area where the oil shale is present. A new detection method is provided for the exploration of oil shale.
文章引用:孙鹏飞, 高铁. 利用重磁对应分析法对负磁异常区内油页岩的推断[J]. 地球科学前沿, 2017, 7(2): 190-201. https://doi.org/10.12677/AG.2017.72021

参考文献

[1] 丁树柏, 邢学文. 油页岩遥感探测技术研究[A]. 见: 新世纪以来遥感应用进展交流研讨会论文集[C]. 北京: 中国遥感应用协会专家委员会, 2011.
[2] Goldstein, M.A. and Strangway, D.W. (1975) Audio Frequency Magnetotellurics with a Grounded Electric Dipole Source. Geophysics, 40, 669-683.
https://doi.org/10.1190/1.1440558
[3] 李帝铨, 何继善. 湘西地区页岩气广域电磁法探测研究[A]. 见: 中国地质学会2014年中国地球科学联合术年会论文集[C]. 北京: 中国地球物理学会, 2014.
[4] 王红岩. 中国油页岩资源分布及技术进展[M]. 北京: 石油工业出版社, 2013: 100-112.
[5] 谷天本. 油页岩地层优化钻进技术研究[D]: [博士学位论文]. 武汉: 中国地质大学, 2011: 1-115.
[6] Abdelrahman, E.M., et al. (1985) On the Least-Squares Residual Anomaly Determination. Geophysics, 50, 473-480.
https://doi.org/10.1190/1.1441925
[7] Chakravarthi, V. and Ramamma, B. (2015) Determination of Sedimentary Basin Basement Epth: A Space Domain Based Gravity Inversion using Exponential Density Function. Acta Geophysica, 63, 1066-1079.
[8] 刘东甲, 程方道. 划分重力区域场与局部场的多次切割法[J]. 物探化探计算技术, 1997, 19(1): 31-35.
[9] 窦喜英, 吴燕冈, 王恩利, 等. 重磁对应分析方法在东北地区实际资料处理中的应用[J]. 吉林地质, 2006, 25(2): 42-47.
[10] 吴燕冈, 窦喜英, 杨春成, 等. 重磁对应分析方法的参数选择及应用[A]. 见: 第二届环境与工程地球物理国际会议论文集[C]. 武汉: 中国地质大学, 2006.
[11] 范正国, 刘前坤, 黄旭钊, 等. 自适应重磁对应分析[J]. 吉林大学学报(地球科学版), 2012, 42(6): 1903-1911.