Study on the Prospecting Direction and Metallogenic Regularity of Granite Porphyry Gold Tungsten Molybdenum Polymetallic Deposits

雷旺胜; 石康伟; 邓林燕

doi:10.16056/j.1005-7676.2015.01.008

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Study on the Prospecting Direction and Metallogenic Regularity of Granite Porphyry Gold Tungsten Molybdenum Polymetallic Deposits

更新时间：2026-01-19

- Study on the Prospecting Direction and Metallogenic Regularity of Granite Porphyry Gold Tungsten Molybdenum Polymetallic Deposits
- Issue 1, Pages: 26-29(2015)
- 作者机构：
  
  陕西省核工业地质局二二四大队
- 作者简介：
- 基金信息：
- DOI：10.16056/j.1005-7676.2015.01.008
  CLC： P618.2
- Published：2015
- 稿件说明：
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[1]雷旺胜,石康伟,邓林燕.花岗斑岩型金钨钼多金属矿成矿规律与找矿方向研究[J].能源研究与管理,2015(01):26-29.

雷旺胜, 石康伟, 邓林燕. Study on the Prospecting Direction and Metallogenic Regularity of Granite Porphyry Gold Tungsten Molybdenum Polymetallic Deposits[J]. 2015, (1): 26-29.
[1]雷旺胜,石康伟,邓林燕.花岗斑岩型金钨钼多金属矿成矿规律与找矿方向研究[J].能源研究与管理,2015(01):26-29. DOI： 10.16056/j.1005-7676.2015.01.008.

雷旺胜, 石康伟, 邓林燕. Study on the Prospecting Direction and Metallogenic Regularity of Granite Porphyry Gold Tungsten Molybdenum Polymetallic Deposits[J]. 2015, (1): 26-29. DOI： 10.16056/j.1005-7676.2015.01.008.

摘要

花岗斑岩型成矿系统通常作为"挤压型"陆缘岩浆弧——"碰撞裂谷带"的典型代表而一直备受关注。近年来的研究表明斑岩型钨钼多金属成矿带都是由一系列深大断裂控制

大型斑岩矿床往往产于深大断裂附近

而裂谷缝合带及两侧的构造岩浆带则是孕育花岗斑岩型金、钨、钼、多金属矿床的重要成矿远景带。通过对斑岩型矿床的成矿规律分析

进一步指导花岗斑岩型金钨钼多金属矿床的找矿方向。

Abstract

Granite porphyry metallogenic system usually has been focued as a typical representative of "squeeze-type"- "Collision rift zone" marginal magma arc. Recent studies show that the porphyry tungsten molybdenum polymetallic metallogenic belt are controlled by a series of deep faults

produced in the vicinity of deep faults

Magmatic rift zone and On either side of the rift valley suture zone is an important metallogenic belt Vision which bred the Granite Porphyry Gold tungsten Molybdenum Polymetallic Deposits. Through the analysis of the metallogenic regularity of porphyry deposits

Further guidance granite porphyry gold prospecting direction of tungsten molybdenum polymetallic deposit.

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