云南澜沧老厂红土型银锰矿床地质特征及成因探讨
本文概述了老厂红土型银锰矿床成矿地质背景，地质特征及成矿规律，提出本矿床总体属初生红土型银锰矿床，成矿作用主要与红土化作用有关，银锰成矿物质主要来源于C2＋3－P1碳酸盐岩，并将银锰次生富集过程划分为四个阶段。...
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| Veröffentlicht in: | Da di gou zao yu cheng kuang xue 2002, Vol.26 (1), p.86-91 |
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| container_title | Da di gou zao yu cheng kuang xue |
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| creator | 陈百友 张映旭 等 |
| description | 本文概述了老厂红土型银锰矿床成矿地质背景，地质特征及成矿规律，提出本矿床总体属初生红土型银锰矿床，成矿作用主要与红土化作用有关，银锰成矿物质主要来源于C2＋3－P1碳酸盐岩，并将银锰次生富集过程划分为四个阶段。 |
| doi_str_mv | 10.3969/j.issn.1001-1552.2002.01.015 |
| format | Article |
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| fulltext | fulltext |
| identifier | ISSN: 1001-1552 |
| ispartof | Da di gou zao yu cheng kuang xue, 2002, Vol.26 (1), p.86-91 |
| issn | 1001-1552 |
| language | chi |
| recordid | cdi_wanfang_journals_ddgzyckx200201015 |
| source | Alma/SFX Local Collection |
| subjects | 云南 地质特征 成矿规律 矿床成因 红土型银锰矿床 |
| title | 云南澜沧老厂红土型银锰矿床地质特征及成因探讨 |
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