中国地质
中國地質
중국지질
CHINESE GEOLOGY
2014年
6期
2048-2062
,共15页
苏旭亮%赵永亮%赵闯%张学明%李恒恒%刘国燕%宋涛涛
囌旭亮%趙永亮%趙闖%張學明%李恆恆%劉國燕%宋濤濤
소욱량%조영량%조틈%장학명%리항항%류국연%송도도
找矿思路%找矿模型%克停哈尔%铜钼矿床%祁漫塔格%东昆仑
找礦思路%找礦模型%剋停哈爾%銅鉬礦床%祁漫塔格%東昆崙
조광사로%조광모형%극정합이%동목광상%기만탑격%동곤륜
prospecting thinking%prospecting model%Ketinghaer%copper molybdenum deposit%Qimantag%East Kunlun Mountains
东昆仑之祁漫塔格成矿带以矿床类型、金属种类丰富多样为特征,以矽卡岩型矿床为典型,是地质学者研究的热点地区之一。近年来此成矿带中的斑岩型铜钼矿找矿不断有新的突破,2013年在该成矿带东侧克停哈尔地区又新发现一典型斑岩型铜钼矿。矿区地层以古元古代金水口岩群为主,岩性为片麻岩、大理岩等变质岩,华力西期、印支期中酸性岩体广泛侵入,后者为赋矿岩石,岩体内有隐伏的小斑岩体及隐爆角砾岩,矿区北西向、北东向构造发育,有多个物化探异常分布。本区找矿突破是在全面认识分析以上成矿地质条件、物化探异常特征,类比已知典型铜钼矿床基础上,初步建立寻找斑岩型矿床的找矿思路,并据此思路开展勘查工作,最终取得了找矿突破,进而总结出克停哈尔斑岩型铜钼矿的找矿思路方法,建立了地质-地球化学-地球物理综合信息找矿模型,为区域上开展同类型矿床的找矿工作提供了思路和方向。
東昆崙之祁漫塔格成礦帶以礦床類型、金屬種類豐富多樣為特徵,以矽卡巖型礦床為典型,是地質學者研究的熱點地區之一。近年來此成礦帶中的斑巖型銅鉬礦找礦不斷有新的突破,2013年在該成礦帶東側剋停哈爾地區又新髮現一典型斑巖型銅鉬礦。礦區地層以古元古代金水口巖群為主,巖性為片痳巖、大理巖等變質巖,華力西期、印支期中痠性巖體廣汎侵入,後者為賦礦巖石,巖體內有隱伏的小斑巖體及隱爆角礫巖,礦區北西嚮、北東嚮構造髮育,有多箇物化探異常分佈。本區找礦突破是在全麵認識分析以上成礦地質條件、物化探異常特徵,類比已知典型銅鉬礦床基礎上,初步建立尋找斑巖型礦床的找礦思路,併據此思路開展勘查工作,最終取得瞭找礦突破,進而總結齣剋停哈爾斑巖型銅鉬礦的找礦思路方法,建立瞭地質-地毬化學-地毬物理綜閤信息找礦模型,為區域上開展同類型礦床的找礦工作提供瞭思路和方嚮。
동곤륜지기만탑격성광대이광상류형、금속충류봉부다양위특정,이석잡암형광상위전형,시지질학자연구적열점지구지일。근년래차성광대중적반암형동목광조광불단유신적돌파,2013년재해성광대동측극정합이지구우신발현일전형반암형동목광。광구지층이고원고대금수구암군위주,암성위편마암、대리암등변질암,화력서기、인지기중산성암체엄범침입,후자위부광암석,암체내유은복적소반암체급은폭각력암,광구북서향、북동향구조발육,유다개물화탐이상분포。본구조광돌파시재전면인식분석이상성광지질조건、물화탐이상특정,류비이지전형동목광상기출상,초보건립심조반암형광상적조광사로,병거차사로개전감사공작,최종취득료조광돌파,진이총결출극정합이반암형동목광적조광사로방법,건립료지질-지구화학-지구물리종합신식조광모형,위구역상개전동류형광상적조광공작제공료사로화방향。
The Qimantag metallogenic belt in the East Kunlun Mountains is characterized by a large variety of deposit types and metallic kinds, with skarn deposits being the typical type. Hence, this belt has become one of the hotspots among geologists. In recent years, the prospecting for porphyry copper molybdenum deposit has achieved new breakthroughs continually in this metallogenic belt. In Ketinghaer, to the east of this belt, a new porphyry copper molybdenum deposit was discovered in 2013. The strata in this area belong mainly to Paleoproterozoic Jinshuikou Group, and the main rocks are metamorphic rocks, such as gneiss and marble. The Variscan and Indosinian intermediate-acidic intrusive rocks are widely distributed in this area, with the Indosinian intrusive rocks being the host rocks;within the rock bodies, there are small porphyry mass and cryptoexplosion breccia. In addition, the NW-, NE-trending structures and multiple geophysical-geochemical anomalies are also distributed in this area. Through a comprehensive analysis of the above conditions including geological conditions, geophysical- geochemical anomalies, and characteristics of typical porphyry copper molybdenum deposits, the authors tentatively summed up the prospecting thinking for porphyry deposits. On such a basis, the prospecting work was carried out, which led to the breakthrough finally. And then, the authors summarized the prospecting thinking and methods for the Ketinghaer porphyry copper molybdenum deposit, and established a geological-geochemical-geophysical comprehensive model so as to provide the train of thought and orientation in search for the same type of deposits in this region.