大地构造与成矿学
大地構造與成礦學
대지구조여성광학
GETECTONICA ET METALLOGENIA
2014年
1期
108-118
,共11页
郑有业%孙祥%田立明%郑海涛%于淼%杨万涛%周天成%耿学斌
鄭有業%孫祥%田立明%鄭海濤%于淼%楊萬濤%週天成%耿學斌
정유업%손상%전립명%정해도%우묘%양만도%주천성%경학빈
北喜马拉雅东段%金锑多金属矿床%成矿作用%矿床类型%成矿时代
北喜馬拉雅東段%金銻多金屬礦床%成礦作用%礦床類型%成礦時代
북희마랍아동단%금제다금속광상%성광작용%광상류형%성광시대
eastern part of North Himalayan%gold antimony polymetallic deposit%mineralization%deposit type%metallogenic age
通过大量详实的野外地质调查与综合研究,结合前人的研究成果,总结出北喜马拉雅东段金锑多金属矿带发育3期成矿作用(同沉积、同碰撞、陆内造山期)和5种矿床类型(喷流沉积-改造型、卡林型-类卡林型、热泉型、次火山岩浆热液型、造山型)。提出控矿“四要素”分布或叠加的地区,是北喜马拉雅地区最重要的找矿标志。指出羊卓雍错-哲古错被动大陆边缘裂谷(陷)盆地周缘的盆山转换部位是成矿有利部位,金矿床主要受近 EW 向拆离构造及其次级构造控制;锑、金锑多金属矿床主要受近SN向走滑正断系统及其次级构造控制,特别是EW向拆离系统与SN向走滑正断系统的交汇部位更是寻找锑、金锑多金属矿床的最有利部位。据此划分出3个受近SN向走滑正断层系统控制和2个受EW向拆离构造或韧-脆性剪切构造控制的矿化集中区,为该带进一步的找矿工作部署与突破指明了方向。
通過大量詳實的野外地質調查與綜閤研究,結閤前人的研究成果,總結齣北喜馬拉雅東段金銻多金屬礦帶髮育3期成礦作用(同沉積、同踫撞、陸內造山期)和5種礦床類型(噴流沉積-改造型、卡林型-類卡林型、熱泉型、次火山巖漿熱液型、造山型)。提齣控礦“四要素”分佈或疊加的地區,是北喜馬拉雅地區最重要的找礦標誌。指齣羊卓雍錯-哲古錯被動大陸邊緣裂穀(陷)盆地週緣的盆山轉換部位是成礦有利部位,金礦床主要受近 EW 嚮拆離構造及其次級構造控製;銻、金銻多金屬礦床主要受近SN嚮走滑正斷繫統及其次級構造控製,特彆是EW嚮拆離繫統與SN嚮走滑正斷繫統的交彙部位更是尋找銻、金銻多金屬礦床的最有利部位。據此劃分齣3箇受近SN嚮走滑正斷層繫統控製和2箇受EW嚮拆離構造或韌-脆性剪切構造控製的礦化集中區,為該帶進一步的找礦工作部署與突破指明瞭方嚮。
통과대량상실적야외지질조사여종합연구,결합전인적연구성과,총결출북희마랍아동단금제다금속광대발육3기성광작용(동침적、동팽당、륙내조산기)화5충광상류형(분류침적-개조형、잡림형-류잡림형、열천형、차화산암장열액형、조산형)。제출공광“사요소”분포혹첩가적지구,시북희마랍아지구최중요적조광표지。지출양탁옹착-철고착피동대륙변연렬곡(함)분지주연적분산전환부위시성광유리부위,금광상주요수근 EW 향탁리구조급기차급구조공제;제、금제다금속광상주요수근SN향주활정단계통급기차급구조공제,특별시EW향탁리계통여SN향주활정단계통적교회부위경시심조제、금제다금속광상적최유리부위。거차화분출3개수근SN향주활정단층계통공제화2개수EW향탁리구조혹인-취성전절구조공제적광화집중구,위해대진일보적조광공작부서여돌파지명료방향。
The deposit type and metallogenic age of the gold antimony polymetallic belt in the eastern part of North Himalayan is poorly constrained. Based on the detailed field geological survey and comprehensive studies, together with the previous researches, the authors propose that this belt experienced three pulses of mineralization during the syn-depositional, syn-collisional and intra-continental periods, respectively. We delineate five types of ore deposits including exhalative sedimentation-reworked, Carlin - Carlin-like, hot spring, subvolcano magmatic hydrothermal, and orogenic types, and point out four ore controlling factors. The crossover of the basin and the mountain in the Lake Yamdrok-Lake Zhegu passive continental margin rift valley is the favorable ore-forming area. The gold deposits are mainly controlled by nearly EW-trending detachment structures and the secondary structures; the antimony and antimony polymetallic deposits are mainly controlled by near SN-trending strike-slip normal faults and the corresponding secondary structures. Particularly, the intersection of the two types of structures is the most favorable prospecting area. Furthermore, we argue that the three mineralization districts are controlled by SN-trending strike-slip normal faults and two mineralization districts are controlled by EW-trending detachment structures, which will be helpful for the prospecting deployment.