摘要
泽当蛇绿岩位于雅鲁藏布江缝合带东段,岩体由地幔橄榄岩、辉长辉绿岩、辉石岩、火山岩等组成。地幔橄榄岩主要为方辉橄榄岩、纯橄岩和二辉橄榄岩。在方辉橄榄岩中发现7处豆荚状铬铁矿,矿石类型主要有致密块状和浸染状。出露地表的长度0.5—3m,厚0.2~1m。矿体的延伸方向为北西向,与岩体展布的方向一致,铬铁矿的Cr#=67.9—88.5,属于高铬型铬铁矿。泽当地幔橄榄岩岩相学特征以及矿物组合、矿物化学成份及岩相学特征,显示岩体至少存在两次的部分熔融过程,即为早期的MOR构造背景,以及后期SSZ环境的改造。铬铁矿的铂族元素(PGE)以富集Os、Rh、Pd,亏损Ir、Ru、Pt的负斜率分布模式,表明其形成过程中经受后期熔体/流体的改造。对比罗布莎岩体的矿物组合,矿物化学和地球化学等特征,显示泽当豆荚状铬铁矿矿体与典型高铬型具相似性,存在较大的找矿空间。
The Zedong ophiolite is in the eastern Yarlung-Zangbo suture zone (YZSZ) of Tibet, which consists chiefly of mantle peridotite, with lesser amounts of pyroxenite and gabbro. Seven small, lenticular bodies of chromitite ore have been found in the harzburgite, with ore textures ranging from massive to disseminate to sparsely disseminate. Individual ore bodies are 0. 5 ~ 3m long, 0. 2 ~ lm wide and striek NW, parallel to the main structure of the peridotite, both of them are high-Cr chromitite ( Cr~ = 67. 9 ~ 88.5 ). The mineralogy and geochemistry of the Zedong peridotites suggest that they formed originally at a mid-ocean ridge (MOR) and were later modified by suprasubduction zone (SSZ) melts. Platinum group elements (PGE) of Zedong ophiolite have negative slope patterns with enrich Os, Rh, Pd, loss of It, Ru and Pt, indicating the process of modified by melt/fluid. Compare to Luobusa podiform chromitite and peridotite in mineral assemblages, mineral chemistry and geochemistry show that there are many similar character, even existence a good prospecting space.
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2016年第12期3635-3648,共14页
Acta Petrologica Sinica
基金
国家行业专项(Sino Probe-05-02)
国家自然科学基金重点项目(40930313)
国家自然科学基金创新群体项目(40921001)
国家自然科学基金项目(41502062
41672046)
国家重点研究计划项目(A1602-4d)
中国地质调查局工作项目(DD20160023
2014DFR2127C)
中国地质科学院地质研究所基本科研业务费(J1526)
IGCP-649项目联合资助
关键词
高铬型铬铁矿
铂族元素
泽当岩体
雅鲁藏布江缝合带
High-Cr chromitite
Platinum group elements
Zedong ophiolite
Yarlung-Zangbo suture zone