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红格层状岩体角闪石和黑云母对温压及氧逸度条件的估算
栾燕; 宋谢炎; 郑文勤; 陈列锰; 田小林; 冉启渝
2013
Source Publication矿物学报
IssueS2Pages:119-119
Abstract前人对攀西地区钒钛磁铁矿形成时的温压和氧逸度条件等进行了一定的分析探讨。Pang等(2008a、b,2009)根据磁铁矿和钛铁矿电子探针成分估计了攀枝花岩体氧化物结晶的温度和氧逸度,但是,由于磁铁矿和钛铁矿都发生了固溶体分离,根据电子探针分析估计的温度和氧逸度具有较大的误差。张晓琪等(2011)则利用攀枝花岩体没有发生固溶体分离的斜长石和橄榄石估算了攀枝花钒钛磁铁矿形成时的温度和氧逸度的相对变化.
Keyword氧逸度 红格 温压 钒钛磁铁矿 电子探针 层状岩体 钛铁矿 攀西地区 邓晋福 辉岩
Indexed ByCSCD
Language中文
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5475
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
栾燕,宋谢炎,郑文勤,等. 红格层状岩体角闪石和黑云母对温压及氧逸度条件的估算[J]. 矿物学报,2013(S2):119-119.
APA 栾燕,宋谢炎,郑文勤,陈列锰,田小林,&冉启渝.(2013).红格层状岩体角闪石和黑云母对温压及氧逸度条件的估算.矿物学报(S2),119-119.
MLA 栾燕,et al."红格层状岩体角闪石和黑云母对温压及氧逸度条件的估算".矿物学报 .S2(2013):119-119.
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