大、小兴安岭北部中生代火山岩区岩金矿床剥蚀程度的初步研究
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本文为中国科学院“知识创新工程”重大项目(编号 KZCX1Y03)与中国科学院“九五”黄金重大项目(编号 KZ951A1404)联合资助。


A Priliminary Study of the Denudation Extent of Mesozoic Vein Gold Deposits of Continental Volcanic Rocks in the Northern Part of the Greater and Lesser Hinggan Mountains, Northeast China
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    摘要:

    大、小兴安岭北部中生代幔源火山岩发育,以中心式喷发为主,砂金分布面积广,是岩金成矿集中区,实现岩金找矿突破的关键是圈定有利的成矿构造部位和最佳保存条件。本文分析了火山岩区地质特征、火山活动的大地构造环境及其与金矿化的关系,从成矿元素组合、砂金成色分布规律、岩金矿床出露高度、残留火山机构等4个方面总结岩金矿床剥蚀程度的判别标志,并指出了岩金找矿方向。

    Abstract:

    The fact that not only mantlesourced Mesozoic volcanic rocks of the central eruption type are well developed in the northern part of the Greater and Lesser Hinggan Mountains but also there is a wide distribution of gold pla cers in the region shows that it is a vein gold metallogenic concentrated region . Therefore, the key to breakthroughs in future exploration is the delineation of the most favorable metallogenic structural posit ions of vein gold deposits and the optimum preservation conditions. By analyzing the geological featuers of the Mesozoic volcanic rocks, the distribution pattern of placer gold , the exposed elevation of vein gold deposits , the residual extents of volcanics, the denudation extent of vein gold depo sits, etc., this paper presents a genetic model of the Mesozoic vein gold d e posits of volcanic rock type and proposes the directions and targets for prospecting.

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张宝林,蔡新平,王 杰,徐兴旺,秦大军,高浩中.1999.大、小兴安岭北部中生代火山岩区岩金矿床剥蚀程度的初步研究[J].地质论评,45(7):414-421,[DOI].
Zhang Baolin, Cai Xinping, Wang Jie, Xu Xingwang, Qin Dajun, Gao Haozhong.1999. A Priliminary Study of the Denudation Extent of Mesozoic Vein Gold Deposits of Continental Volcanic Rocks in the Northern Part of the Greater and Lesser Hinggan Mountains, Northeast China[J]. Geological Review,45(7):414-421.

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