Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust | |
Li, Ji-Lei1; Klemd, Reiner1; Gao, Jun2; Meyer, Melanie1 | |
刊名 | AMERICAN MINERALOGIST |
2014 | |
卷号 | 99期号:1页码:206-217 |
关键词 | Prograde zoning dolomite magnesite eclogite high pressure Tianshan |
ISSN号 | 0003-004X |
DOI | 10.2138/am.2014.4507 |
文献子类 | Article |
英文摘要 | Dolomite with compositional zoning was discovered in carbonate-lawsonite-bearing eclogites in the Tianshan (ultra-)high-pressure/low-temperature metamorphic belt, northwestern China. The eclogite-facies dolomite occurs as matrix porphyroblast and as inclusion in garnet, both of which display the same chemical zoning pattern. The dolomite contains inclusions of calcite (probably after aragonite), magnesite, glaucophane, lawsonite (and its pseudomorphs), allanite, epidote, paragonite, phengite, and omphacite. The chemical zoning in dolomite is well defined by a continuous core-to-rim Mg increase and Fe-Mn decrease. The concentrations of transition metal elements, REE, and Y also decrease from core to rim of the dolomite. Thermodynamic modeling demonstrates that the Fe-Mg zoning of dolomite is largely temperature dependent and, thus, is interpreted as prograde growth zoning, which developed during subduction of carbonate-bearing oceanic crust. It is suggested that dolomite in equilibrium with garnet formed as a result of changing matrix compositions due to increasing temperatures. In addition, thermodynamic modeling demonstrates that during subduction at high-pressure conditions prograde-formed aragonite and dolomite were transformed to dolomite and magnesite. Furthermore, Fe-rich magnesite inclusions in matrix dolomite and in dolomite inclusions in garnet are shown to have formed during high-pressure conditions prior to peak metamorphic conditions and, therefore caution is warranted using Fe-bearing magnesite occurrences in eclogite-facies rocks as an unambiguous ultrahigh pressure indicator as previously suggested. |
WOS关键词 | HIGH-PRESSURE METAMORPHISM ; FLUID-ROCK INTERACTION ; HP-LT ROCKS ; WESTERN TIANSHAN ; NW-CHINA ; PHASE-RELATIONS ; TECTONIC IMPLICATIONS ; COESITE INCLUSIONS ; AGE CONSTRAINTS ; DABIE MOUNTAINS |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
出版者 | MINERALOGICAL SOC AMER |
WOS记录号 | WOS:000329416700026 |
资助机构 | Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation of China(41025008) ; National Natural Science Foundation of China(41025008) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation of China(41025008) ; National Natural Science Foundation of China(41025008) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation of China(41025008) ; National Natural Science Foundation of China(41025008) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation of China(41025008) ; National Natural Science Foundation of China(41025008) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/86482] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Li, Ji-Lei |
作者单位 | 1.Univ Erlangen Nurnberg, GeoZentrum Nordbayern, D-91054 Erlangen, Germany 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Ji-Lei,Klemd, Reiner,Gao, Jun,et al. Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust[J]. AMERICAN MINERALOGIST,2014,99(1):206-217. |
APA | Li, Ji-Lei,Klemd, Reiner,Gao, Jun,&Meyer, Melanie.(2014).Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust.AMERICAN MINERALOGIST,99(1),206-217. |
MLA | Li, Ji-Lei,et al."Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust".AMERICAN MINERALOGIST 99.1(2014):206-217. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论