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顽火辉石球粒陨石GRV 13100两类球粒和NWA 13632热变质历史对比

高旭凯 谢兰芳 陈宏毅 杨姗姗 夏志鹏 殷一曼 赵妍菲

极地研究2025,Vol.37Issue(3):510-521,12.
极地研究2025,Vol.37Issue(3):510-521,12.DOI:10.13679/j.jdyj.20240044

顽火辉石球粒陨石GRV 13100两类球粒和NWA 13632热变质历史对比

Comparison of the thermal metamorphic history between two types of chon-drules in GRV 13100 and NWA 13632 enstatite chondrites

高旭凯 1谢兰芳 1陈宏毅 2杨姗姗 3夏志鹏 1殷一曼 1赵妍菲1

作者信息

  • 1. 桂林理工大学行星地质演化广西高校重点实验室 陨石与行星物质研究中心,广西 桂林 541006||桂林理工大学广西隐伏金属矿产勘查重点实验室,广西 桂林 541006
  • 2. 桂林理工大学行星地质演化广西高校重点实验室 陨石与行星物质研究中心,广西 桂林 541006||桂林理工大学有色金属矿产勘查与资源高效利用省部共建协同创新中心,广西 桂林 541004
  • 3. 中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广东 广州 510640
  • 折叠

摘要

Abstract

The characteristics of petrology and mineralogy for porphyritic olivine pyroxene chondrule and barred pyroxene chondrule in GRV 13100(EH4)and the whole rock in NWA 13632(EH6)enstatite chondrite are reported in this paper,and the comparative study of their thermal metamorphic history are carried out.Two different cathodolumine-scence olivine,thermometers of oldhamite of porphyritic olivine pyroxene chon-drule in GRV 13100 show that the chondrule have undergone incomplete melting of 800~900℃and rapid cooling crystallization.The barred pyroxene chondrule in GRV 13100 underwent complete high-temperature melting higher than 1315℃,and the cooling rate was greater than 1 000℃·h-1.Their thermal metamorphic characteristics conform to the"rubble pile model",and the metamorphic heat source comes from the impact energy.NWA 13632 enstatite chondrite has a high degree of thermal metamorphism(type 6)and weathering(W3),a blurred boundary between chondrule and matrix,a low impact metamorphism(S2),no impact melt-ing phenomenon;The olivine and silica phases are absent in the residual spherules and matrix.Compared with GRV 13100,the Mn content of enstatite and troilite in NWA 13632 is low,and the secondary plagio-clase and pyroxene form an equigranular texture in some areas.So,its thermal metamorphism characteristics are consistent with the"onion model".NWA13632 meteorite may have formed deep within its parent body and was heated by the decay of radioactive elements.

关键词

顽火辉石球粒陨石/岩石学/矿物学/热变质/GRV 13100/NWA 13632

Key words

enstatite chondrite/petrology/mineralogy/thermal metamorphism/GRV 13100/NWA 13632

引用本文复制引用

高旭凯,谢兰芳,陈宏毅,杨姗姗,夏志鹏,殷一曼,赵妍菲..顽火辉石球粒陨石GRV 13100两类球粒和NWA 13632热变质历史对比[J].极地研究,2025,37(3):510-521,12.

基金项目

国家自然科学基金(42473051)、广西自然科学基金(2025GXNSFAA069991)、广西科技基地与人才专项(桂科AD23026339)和桂林理工大学科研启动金(RD2400003226)资助 (42473051)

极地研究

OA北大核心

1007-7073

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