单斜构造区岩溶倾斜洞穴发育趋势与岩层产状相关性识别

罗书文; 杨 桃; 陈伟海; 邓亚东; 潘晓东; 陈宏峰; 李成展

doi:10.11932/karst20180315

单斜构造区岩溶倾斜洞穴发育趋势与岩层产状相关性识别

doi: 10.11932/karst20180315

1.
中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室
2.
贵阳十二中学

基金项目: 中国地质科学院院长基金（YYWF201638）；岩溶地质研究所所长基金（2014022）；中国地质调查工作项目（基201201009018、2015040301016、1212011220049）；广西科技公关计划（14124004-4-6）

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出版历程
- 发布日期: 2018-06-25

Relationship between development of inclined karst cave and bedrock orientation in a monoclinal structure area

1.
Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR&GZAR
2.
Guiyang No.12 Middle School

摘要

摘要: 通过构建岩溶倾斜洞穴发育趋势面和岩层倾向面，探讨在单斜构造区岩溶倾斜洞发育趋势与岩层产状的相关性。首先，根据洞穴探测导线长度、方向、倾角等要素，以测量初始点为原点建立空间直角坐标系，将测量空间方位角转换为平面直角坐标系中的方向角，将测量数据投影在平面直角坐标系上，运用向量加法原理求出各测点平面向量及坐标，结合各测点的相对高差,运用趋势面分析方法进行一次拟合，构建洞道空间展布平面方程；其次，根据岩层产状信息在空间坐标系中构建平面方程；最后，通过计算两平面法向量的夹角，来判断洞穴空间展布平面和岩层产状平面的重合度，同时求出两平面与同一水平面的交线所成角来判断洞穴空间展布趋势面与岩层面的倾向关系。通过实例证明，该方法用于探讨单斜构造区岩层产状对倾斜洞穴发育趋势的影响识别具有一定的实用性。
- 单斜构造 /
- 倾斜洞穴 /
- 发育趋势 /
- 岩层产状 /
- 相关性分析
Abstract: In this paper, the relationship between the developmental trend of karst inclined cave and the orientation of rock formation in monoclinal structural area by constructing cave spatial distribution trend surface and rock dipping surface. Firstly, measurement initial point is regarded as original point for establishment of spatial Cartesian coordinate system according to cave exploration wire length, direction, inclination and other factors. The measurement wire is projected on the plane so that the spatial azimuth is converted to orientation angle in plane rectangular coordinate system, and the angle values are calculated. Principle of vector addition is used for calculating plane vectors and coordinates of each measured point. Relative elevation difference of each measuring point is recorded, trend surface analysis method is utilized for primary fitting, which could construct channel space distribution plane equation. Secondly, the plane equation is constructed in spatial coordinate system according to the rock orientation information. Finally, the coincidence degree of cave spatial distribution plane and rock occurrence plane is judged by calculating the angle between two plane normal vectors. Meanwhile, the trend relationship between cave spatial distribution trend surface and rock surface is judged by the angle formed by two planes and crossed line on the same level. Example analysis shows that the method is used for investigating quantitative analysis between karst cave spatial distribution and rock correlation with certain practicality and scientific value.
- monoclinal structure /
- inclined cave /
- developmental trend /
- rock occurrence /
- correlation analysis

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参考文献(22)

[1]	Mylroie J E. Hydrologic classification of caves and karst［M］.In:Groundwater as a geomorphic agent, edited by:R G,La Fleur,Allen & Unwin,Inc.,Boston,MA,1984:157-172.
[2]	Bogli A.Karst hydrology and speleology［M］.Berlin:Springer,1980.
[3]	张庆玉,梁彬,淡永,等.塔中北斜坡奥陶系鹰山组岩溶储层特征及古岩溶发育模式［J］.中国岩溶,2016,35(1): 106-113.
[4]	Ewers R O. Cavern development in the dimensions of length and breadth［D］. Mc Master University,1982.
[5]	Ford D C,Ewers R O. The development of limestone cave systems in the dimensions of 1ength and breadth［J］. Canadian Journal of Earth Science,1978,15(11):1783-1798.
[6]	Derek Fodr,Paul Williarns.Karst geomorphology and hydrology［M］.London:Unwin Hyman,1989.
[7]	Randall C Orndorff, David J Weary, Stanka Sebela. Geologic Framework of the Ozarks of South-Central Missouri—Contributions to a Conceptual Model of Karst［R］. Water-Resources Investigations Report 01-4011, 2001:18-24.
[8]	陈鸿汉，曹以临.吉林省通化鸭园洞穴系统特征及形成与遗存机理［J］. 中国岩溶, 1991,10（2）：162-170.
[9]	Howard A D. Quantiative measures of cave patterns［J］. Cave and Karst, 1971,13(1):1-7.
[10]	李文兴.岩溶洞穴长度空间形态的分形研究［J］. 广西科学,1998,5(3):237-240.
[11]	Curl R L. Fractal dimensions and geometries of caves［J］. Mathematical Geology，1986 ，18(8): 765-783.
[12]	Mace R E , Marrett R, Hovorka S. Fractal scaling of secondary porosity in karstic exposures of the Edwards Aquifer:Sinkholes and the Engineering and Environmental Impacts of Karst［M］. ASCE, Geotechnical Special Publication 144, Proceeding of the Tenth Multidisciplinary Conference, 2005:1-10.
[13]	Pardo-Igtlzquiza  E, Durcin-Valsero J J , Rodriguez-Galiano V. Morphometric analysis of three-dimensional networks of karst conduits［J］. Geomorphology，2011，132（3）：17-28.
[14]	Jeannin P Y , Groves C , Hiiuselaman P. Speleological investigations in Methods in Karst Hydrogeology edited by Nico Goldscheider and David Drew ［M］. London: Taylor &Francis，2007:264.
[15]	朱德浩. 岩溶洞穴成因研究和实验研究综述［J］. 中国岩溶，1993，12(3):285-291.
[16]	罗书文,张远海，史文强，等. 巴马帝皇宫景区地质遗迹特征与旅游开发建议［J］.南方国土资源,2013,3(1):34-36.
[17]	张美良, 林玉石, 冉景成, 等. 贵州荔波岩溶洞穴发育特征［J］. 中国岩溶, 2000,19(1):15-20.
[18]	罗书文, 刘一玲, 邓亚东, 等. 四川洪雅县瓦屋山燕子洞探测与形成研究［J］. 国土与自然资源研究,2014,85(3):85-87.
[19]	邓自强. 桂林岩溶洼地和洞穴发生、发展的构造控制剖析［J］. 中国岩溶，1987, 6(2):137-149.
[20]	张超, 杨秉庚. 计量地理学（第二版）［M］. 北京：高等教育出版社,1995.
[21]	孙振绮, 张宪君. 空间解析几何与线性代数［M］. 北京：机械工业出版社,2011.
[22]	徐建华.现代地理学中的数学方法［M］.北京：高等教育出版社,2004