CAJ | 학술논문

通过对槐树坪金矿区 F29赋矿断裂构造性质的综合分析，本文认为 F29断裂属于浅部层次的断裂构造，总体上显示张性-张扭性断裂构造特征，有利于成矿物质的沉淀聚集，但延伸程度有限，延深小于1000 m。F29赋矿断裂构造带内金矿化较好，其形态不规则，具张性断裂特征，带内可见大量角砾岩、擦痕、断层泥，呈现出多期次构造活动的特点。该构造带内矿化阶段划分为三个阶段，最后一个阶段晚期的张性构造活动为 Au 矿化的主要成矿阶段。F29断裂构造力学性质表明，该断裂构造经历过多期构造应力场变化，伴随构造应力场变化出现张扭-压扭交替式构造运动，具复合性断裂构造性质。
통과대괴수평금광구 F29부광단렬구조성질적종합분석，본문인위 F29단렬속우천부층차적단렬구조，총체상현시장성-장뉴성단렬구조특정，유리우성광물질적침정취집，단연신정도유한，연심소우1000 m。F29부광단렬구조대내금광화교호，기형태불규칙，구장성단렬특정，대내가견대량각력암、찰흔、단층니，정현출다기차구조활동적특점。해구조대내광화계단화분위삼개계단，최후일개계단만기적장성구조활동위 Au 광화적주요성광계단。F29단렬구조역학성질표명，해단렬구조경력과다기구조응력장변화，반수구조응력장변화출현장뉴-압뉴교체식구조운동，구복합성단렬구조성질。
By?analyzing?its?properties,?F29?fracture?structure?is?the?shallow?level?fracture?structure,?and?shows?the?character?of?transtensional-compression?and?torsion?fracture?structure.?This?is?good?for?precipitation-accumulation?of?metallogenic?materials,?but?its?extendible?extent?may?be?limit,?and?the?extendible?extent?is?possibly?less?than?1000?meters.?Au?mineralization?of?fracture?structure?zone?of?F29?hosting?ore?is?good.?The?fracture?structure?zone?is?irregular?shape,?and?its?activity?has?the?feature?of?tensional?fracture.?There?are?a?lo?of?breccias,?scratches,?and?fault?gouge?to?show?the?character?of?multistage?structure?movement.?The?mineralization?stage?of?the?structure?zone?is?divided?into?three?stages.?The?last?stage?is?late?tensional?structure?movement,?and?this?is?the?main?metallogenic?stage.?The?mechanical?properties?of?F29?fracture?structure?show?it?suffers?several?change?of?multistage?structure?stress?field,?accompanying?altering?transtensional-compression?and?torsion?structure?movement,?and?has?the?complex?fracture?structure?properties.