GYIG OpenIR  > 矿床地球化学国家重点实验室  > 期刊论文
个旧超大型锡多金属矿床成矿物质来源的铅和硫同位素示踪
张欢; 高振敏; 马德云; 陶琰; 伍孟银
2005
Source Publication地质与勘探
Issue2Pages:17-20
Other Abstract文章通过对个旧超大型锡多金属矿床的铅、硫同位素地球化学特征的系统研究,揭示矿床成矿物质具有多来源的特点,矿床的形成是多种成矿作用过程叠加的结果,具有多来源,多期次成矿特点,经历了中三叠世的海底热水沉积作用和燕山晚期岩浆热液的叠加改造作用,个旧超大型锡多金属矿床应为同生沉积与岩浆热液叠加、改造的复合成因矿床。
Keyword个旧 矿质来源 多种成矿作用 热水沉积 岩浆热液
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:1914436
Citation statistics
Cited Times:11[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7422
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
张欢,高振敏,马德云,等. 个旧超大型锡多金属矿床成矿物质来源的铅和硫同位素示踪[J]. 地质与勘探,2005(2):17-20.
APA 张欢,高振敏,马德云,陶琰,&伍孟银.(2005).个旧超大型锡多金属矿床成矿物质来源的铅和硫同位素示踪.地质与勘探(2),17-20.
MLA 张欢,et al."个旧超大型锡多金属矿床成矿物质来源的铅和硫同位素示踪".地质与勘探 .2(2005):17-20.
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