| 关于中条山胡－篦型铜矿床成矿期和成矿时代问题 |
| |
| 引用本文： | 胡维兴.关于中条山胡－篦型铜矿床成矿期和成矿时代问题[J].华北地质矿产杂志,1994(2). |
| |
| 作者姓名： | 胡维兴 |
| |
| 作者单位： | 地矿部天津地质矿产研究所 |
| |
| 摘 要： | 胡－蓖型铜矿床成因，归纳起来可分为沉积－再造和构控－热液两种观点，但二者也有共同之处：一是层控性，二是分为早期细脉浸染型和晚期脉型两种矿化类型。早期矿化为成岩分异或变质分异的产物，生成在２０５９～１９００Ｍａ之间；晚期矿化则是在细脉浸染型矿化的基础上，受中条运动构造－热事件的改造形成，时间在１９００～１８５０Ｍａ之间，二者均属早元古代，而与中元古代西阳河期岩浆－热事件无关。
|
| 关 键 词： | 早期细脉浸染型矿化，晚期脉型矿化，中条运动构造－热事件，早元古代成矿 |
ON MINERALIZATION PERIOD AND METALLOGENIC EPOCH OF THE HU-BI TYPE COPPER CEPOSITS IN ZHONGTIAO MOUNTAINS |
| |
| Authors: | Hu Weixing |
| |
| Institution: | Tianjin Institute of Geology and Mineral Resources |
| |
| Abstract: | View points about genesis of the Hu-Bi type copper deposits may be summarized as twomajor ones,i.e. sedimentation-remoulded mineralization and structural control-hydrothemalorigin.However,they have something in common,e.g. the stratabound characteristics andtwo main mineralization periods,Ore of the early period is veinlet-disseminated type formedby diagenetic or metamorphic differentiation in 2059-l900 Ma,and that of the late period isvein type forrned by remoulding of the early ore due to structural-thermal event of theZhongtiao movement in 1900-l850 Ma,Both type belong to Early-proterozoic rather thanMid-proterozoic and are out of all relation to magma-thermal event of the Xiyanghe epoch. |
| |
| Keywords: | early veinlet-disseminated ore late vein ore structural-thermal event ofZhongtiao Movement Early Proterozoic metallogenesis |
| 本文献已被 CNKI 等数据库收录！ |
