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基性-超基性岩浆成岩和成矿过程中Soret效应的研究进展
朱丹; 罗泰义; 宋谢炎; 义刚; 陶琰; 黄智龙
2007
Source Publication矿物学报
Volume27Issue:3Pages:265-272
metadata_24其它
Abstract综述了当前对基性-超基性岩床和层状岩体的边缘反转现象的传统解释模型,包括围岩混染、岩浆多期注入、岩浆分层、过冷却、晶体沉降、流动分异、结晶和成分对流以及逐渐减少的颗粒间熔体量。详细论述了这些模型的优缺点,认为Soret效应是目前对边缘反转现象比较合适的解释,讨论了中国峨眉山大火成岩省朱布岩体的Soret成矿现象.
Keyword基性-超基性岩
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization国家重点基础研究发展计划(2007CB411401);国家自然科学基金(40572054;40274027;40573020)
Indexed ByCSCD
Language中文
CSCD IDCSCD:3057086
Citation statistics
Cited Times:5[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/497
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
朱丹,罗泰义,宋谢炎,等. 基性-超基性岩浆成岩和成矿过程中Soret效应的研究进展[J]. 矿物学报,2007,27(3):265-272.
APA 朱丹,罗泰义,宋谢炎,义刚,陶琰,&黄智龙.(2007).基性-超基性岩浆成岩和成矿过程中Soret效应的研究进展.矿物学报,27(3),265-272.
MLA 朱丹,et al."基性-超基性岩浆成岩和成矿过程中Soret效应的研究进展".矿物学报 27.3(2007):265-272.
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