新疆托里县科克火热金矿区成矿地质特征

Metallogenic geological characteristics of Kirk hot gold deposit in Tori County, Xinjian

新疆托里县科克火热金矿区区域内地层有多种,从老到新出露地层可以分为中泥盆统库鲁木迪组（D_2k）、中泥盆统巴尔雷克组（D_2b）等七层。区域内部主要是由酸性-中酸性岩浆岩组成的,还有少部分是主要岩性为钾长花岗岩、斜长花岗岩、二长花岗岩、黑云母钾长花岗岩等岩石,岩浆岩侵位的最高层位是石炭系。此外,此区域是北东向的构造,另外本区的基本构造格架是由自南向北发育的达尔布特断裂、安齐断裂、哈图断裂和别鲁阿嘎希断裂构成的。本文还将介绍该区域的地质特征,希望对勘查人员提供参考。

Kirk Tori of Xinjiang county regional hot mainland gold deposit layer has various, from old to new strata can be divided into the Middle Devonian Kuru Mudi group （D2k）, Middle Devonian Barr Lake group （D2b） seven. Within the region is mainly composed of acidic intermediate acidic magmatite, and a small part is the main lithology moyite, plagioclase granite, two granite, biotite K-feldspar granite, magmatite emplaced in Carboniferous strata are the highest. In addition, this area is the ne structure, the basic tectonic framework in this area is composed of Dahl, from the south to the north of the bout fracture development and fracture safety Hatu and Bie Lou Agha F faults. This paper will also introduce the geological features of the region, and hope to provide reference for the exploration personnel.