CAJ | 학술논문

阳山金矿带位于西秦岭南亚带，区内构造复杂，断裂发育较多。安坝断裂带的岩性主要为含炭泥质千枚岩、蚀变斜长花岗斑岩、砾岩、灰岩，而断裂带内的填充物主要为碎裂岩、构造砾岩组成，它们在电性方面表现为低电阻率，为开展高密度电法、瞬变电磁法的开展提供了先决条件。运用该方法结合地质观察，通过断裂带上的某剖面进行解释，最终经钻孔验证，对该区的断裂的勘探具有较好的效果，为下一步的工作提供了较好的指导。
양산금광대위우서진령남아대，구내구조복잡，단렬발육교다。안패단렬대적암성주요위함탄니질천매암、식변사장화강반암、력암、회암，이단렬대내적전충물주요위쇄렬암、구조력암조성，타문재전성방면표현위저전조솔，위개전고밀도전법、순변전자법적개전제공료선결조건。운용해방법결합지질관찰，통과단렬대상적모부면진행해석，최종경찬공험증，대해구적단렬적감탐구유교호적효과，위하일보적공작제공료교호적지도。
The Yangshan gold ore belt lies in the south zone of West Qinling Mountains where structure is very complicated with development of faults. The Anba fracture is composed of carbonaceous phyllite, altered granite porphyry, limestone, conglomerate with infilling of cataclasite and tectonic breccia. They are characterized by low resistivity in conductive property which provides the possibility for Multi-channel resistivity method and TEM. This paper deals with the application of multi-channel resistivity method and TEM to the Yangshan Au deposit.