煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2015年
3期
11-14
,共4页
瓦乌斯煤矿%构造分析%应力场%断层%判定
瓦烏斯煤礦%構造分析%應力場%斷層%判定
와오사매광%구조분석%응력장%단층%판정
Wawusi mine%tectonic analysis%stress field%fault%judgment
瓦乌斯矿区(盆地)是一个NW走向、南北均为断层边界的断陷含煤盆地,通过电法工作,发现该矿区煤层露头附近视电阻率等值线密集,推断存在走向断层 DF2,但该断层究竟存在与否?产状如何?争议很大。文章基于岩体变形破坏的摩尔强度原理,应用节理应力场分析、赤平投影和断裂共生组合的构造分析方法,判断DF2断层是矿区断裂共生组合中第2序次断裂中的一支,并确定了该断层的产状,结合DF2附近的岩层厚度及变形等特征综合判定了DF2断层的存在。该研究结果对中新生代断陷含煤盆地的构造分析和该矿区煤炭普查工作有积极的指导意义。
瓦烏斯礦區(盆地)是一箇NW走嚮、南北均為斷層邊界的斷陷含煤盆地,通過電法工作,髮現該礦區煤層露頭附近視電阻率等值線密集,推斷存在走嚮斷層 DF2,但該斷層究竟存在與否?產狀如何?爭議很大。文章基于巖體變形破壞的摩爾彊度原理,應用節理應力場分析、赤平投影和斷裂共生組閤的構造分析方法,判斷DF2斷層是礦區斷裂共生組閤中第2序次斷裂中的一支,併確定瞭該斷層的產狀,結閤DF2附近的巖層厚度及變形等特徵綜閤判定瞭DF2斷層的存在。該研究結果對中新生代斷陷含煤盆地的構造分析和該礦區煤炭普查工作有積極的指導意義。
와오사광구(분지)시일개NW주향、남북균위단층변계적단함함매분지,통과전법공작,발현해광구매층로두부근시전조솔등치선밀집,추단존재주향단층 DF2,단해단층구경존재여부?산상여하?쟁의흔대。문장기우암체변형파배적마이강도원리,응용절리응력장분석、적평투영화단렬공생조합적구조분석방법,판단DF2단층시광구단렬공생조합중제2서차단렬중적일지,병학정료해단층적산상,결합DF2부근적암층후도급변형등특정종합판정료DF2단층적존재。해연구결과대중신생대단함함매분지적구조분석화해광구매탄보사공작유적겁적지도의의。
Wawusi mining area (coal-bearing basin) is a faulted depressed coal-bearing basin of NW strike with faults as boundary in both the south and the north. By resistivity method, we discovered that the contour line of apparent resistivity is the densest around the outcrops of coal seams in the mining area, and we inferred the direc-tional fault (DF2). However, two questions are very controversial: whether the fault exists, and how the occurrence of the fault is. In this paper based on Mohr strength theory of rock mass deformation and failure, we made use of joint stress field analysis, hemispherical projection method and fault assemblage analysis to infer that the fault(DF2) is a part of the second fault, and determined the occurrence of the fault (DF2). Also, we took advantage of thickness of strum and deformation features and so on around the fault (DF2) to judge the existence of the fault (DF2). The result has a positive guiding significance for structural analysis in coal-bearing faulted basin of middle Cenozoic and the general coal reconnaissance in the mining area.