[1]陈子龙,彭省临.1992.论粤北多因复成铅锌多金属矿与韶关-四会古断拉谷间的成因关系.大地构造与成矿学,16(2):159-160.
 CEN Zilong PENG Shenglin.1992.ON THE RELATIONSHIP BETWEEN POLYGENETIC COMPOUND Pb-Zn-POLYMETAL DEPOSITS IN NORTHERN GUANGDONG PROVINCE AND THE SHAOGUNG-SHIHUI ANCIENT AULACOGEN.Geotectonica et Metallogenia,16(2):159-160.
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论粤北多因复成铅锌多金属矿与韶关-四会古断拉谷间的成因关系
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
1992年16卷02期
页码:
159-160
栏目:
出版日期:
1992-05-15

文章信息/Info

Title:
ON THE RELATIONSHIP BETWEEN POLYGENETIC COMPOUND Pb-Zn-POLYMETAL DEPOSITS IN NORTHERN GUANGDONG PROVINCE AND THE SHAOGUNG-SHIHUI ANCIENT AULACOGEN
作者:
陈子龙; 彭省临;
中南工业大学地洼学说成矿学研究所; 中南工业大学地洼学说成矿学研究所 长沙 410013; 长沙 410013;
Author(s):
CEN Zilong PENG Shenglin
Institute of Diwa theory metallogey, CSUT, Changsha, 410013
关键词:
铅锌多金属矿床 多因复成 成因关系 黄铁矿 成矿作用 伴生组分 成矿物质 矿床系列 地洼盆地 生长断层
摘要:
粤北地区分布着数十个以铅锌为主的伴生组分众多的多金属矿床或矿点。尽管这些矿床(点)的规模相差悬殊,其主岩层位不一,各矿床(点)之间伴生有用组分的种类和富集的程度不同,但它们仍具有一系列共同的基本特点:(1)产出范围严格限于曲仁

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更新日期/Last Update: 2011-04-29