本文選題：喇嘛蘇外圍　切入點(diǎn)：原生暈　出處：《地質(zhì)論評(píng)》2017年01期 　論文類型：期刊論文

【摘要】：新疆博樂市喇嘛蘇外圍地區(qū)地表巖石風(fēng)化剝蝕嚴(yán)重,直接找礦標(biāo)志不明顯,以大功率激電中梯測(cè)量為輔助功能的大比例尺巖石地球化學(xué)測(cè)量方法對(duì)發(fā)現(xiàn)和圈定隱伏礦體起到了重要作用。根據(jù)化探原生暈元素組合特點(diǎn)及空間分布特征,以單元素異常下限值和富集系數(shù)為劃分標(biāo)準(zhǔn),圈定了六個(gè)Ⅲ級(jí)化探異常帶,異常評(píng)價(jià)初步認(rèn)為Cu—Zn—Pb—Ag—W—Sn—Mn—As—Au—Bi多元素疊加異常的形成為找礦有利區(qū),選元素共生組合特點(diǎn)較明顯的異常帶開展大功率激電工作進(jìn)行化探異常的驗(yàn)證。在推斷出的成礦有利部位布設(shè)鉆孔并可見到礦體。
[Abstract]:The weathering and denudation of the surface rocks in the outer area of Lamasu, Bole City, Xinjiang, is serious, and the direct prospecting marks are not obvious. The method of large scale rock geochemistry survey with high power ionization ladder as auxiliary function has played an important role in the discovery and delineation of concealed orebodies. According to the characteristics of geochemical primary halo element assemblage and spatial distribution, the geochemistry method of large scale rock geochemistry has played an important role in the discovery and delineation of concealed orebodies. Based on the criterion of the lower limit value of single element anomaly and enrichment coefficient, six geochemical anomaly zones of grade 鈪，

本文編號(hào)：1582418