CAJ | 학술논문

槐树坪金矿区位于熊耳山断隆和谭头-嵩县新生代断陷盆地之间，研究表明，中-新生代缓倾斜滑脱拆离断层的次级缓倾斜断裂为槐树坪金矿成矿提供了良好的赋矿空间。矿区揭露的燕山期花岗斑岩体（或隐伏斑岩体）是含矿热液的提供者，含矿热液在适宜的物理化学条件下，沿矿脉或断裂上升至次级缓倾斜断裂中沉淀且富集成矿，矿床规模已达大型。中-新生代缓倾斜滑脱拆离断层属区域大断裂，其次级缓倾斜断裂广泛发育在嵩县南部和洛宁等地区，是有利的赋矿空间，综上可见，缓倾斜次级断裂在区域上的找矿前景非常广阔。
괴수평금광구위우웅이산단륭화담두-숭현신생대단함분지지간，연구표명，중-신생대완경사활탈탁리단층적차급완경사단렬위괴수평금광성광제공료량호적부광공간。광구게로적연산기화강반암체（혹은복반암체）시함광열액적제공자，함광열액재괄의적물이화학조건하，연광맥혹단렬상승지차급완경사단렬중침정차부집성광，광상규모이체대형。중-신생대완경사활탈탁리단층속구역대단렬，기차급완경사단렬엄범발육재숭현남부화락저등지구，시유리적부광공간，종상가견，완경사차급단렬재구역상적조광전경비상엄활。
Huaishuping gold area is located between the Xiong’er Mountain fault and the rift basin of Tantou-Songxian in Cenozoic,research shows that the secondary gentle-dipping faults of gentle dip slip-detachment fault in Meso-Cenozoic has provides the ore-hosting sites for ore-forming of the Huaishuping gold deposit.The Yanshan granite porphyry (or buried porphyry) which revealed has provided the ore-forming fluids.Hydrothermal along veins or fracture rise to secondary gentle-dipping faults and enrichment and mineralization of gold under optimal physical and chemical conditions.The scale of Huaishuping gold deposit has reached large size.The gentle dip slip-detachment fault in Meso-Cenozoic is regional faults and their secondary gentle-dipping faults are widely developed in the south of Songxian and Luoning and so on and offer space for enrichment of metallogenic materials.Comprehensive studies have shown that the secondary gentle-dipping faults on the regional prospecting are very wide.