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Isoplatinocopper,a new mineral,has been found in a bistagite-pyroxene amplhibolite intrusive in the Yenshan Region,China,This mineral has been identified to be isometric and pale yellowish-white in color with a molecular formula of Pt4Cu5,α0=3.786A,specifie gravity=14.5,and no magnetism.In reflected light it is essentially isotropic,and yellowish-white in eclor with reflective power being 58% for green light,61% for yellow and 61.5% for red respectively,and its microhardness 127-220kg/mm^2.On the ground of the data on their chemical composition and crystal structure,Pt-Fe-Cu and Pt-Cu platinum minerals are divisible into two types,i.e.tulameenite which includes those with a composition of Pt5Fe4Cu-Pt2Fe3Ci2 and Pt2FeCu,and isoplatinocopper which possesses a composition of Pt4Cu4-Pt4Cu5.5 相似文献
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Petrology, chronology and isotope geochemistry of the proterozoic amphibolites from Xiangshan, central Jiangxi province, China 总被引:2,自引:0,他引:2
On the basis of a comprehensive study on the petrology,trace elements and isotopic geochemistry of the Xiangshan amphibolites,we suggest that the protoliths of the amphibolites were basalts formed in an island-arc tectonic setting.The basaltic magma was derived from a slightly depleted mantle source with a small amount of crustal contamination.Assemblage of the rock-froming minerals indicates that these amphibolites underwent a low-grade metamorphism of amphibolite facies.According to the formation age(1113Ma) and subsequent metamophic age(726.6Ma) of the basalts aw well as the geological and gochemical features of these amphibolites,a tectonic model of Proterozoic oceanic island-arc setting is proposed for central Jiangxi. 相似文献
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Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Dating of Amphibolites in the Songshugou Ophiolite in the Eastern Qinling 总被引:3,自引:0,他引:3
LIU Liang CHEN Danling ZHANG An ZHANG Chengli YUAN Honglin LUO Jinhai The Key Laboratory of Continental Dynamics Department of Geology Northwest University Xi''an Shaanxi 《《地质学报》英文版》2004,78(1):137-145
Geochemical studies on the arnphibolites in the Songshugou ophiolite from Shangnan County, Shaanxi Province demonstrate that the protolith of the amphibolites is tholeiitic. The arnphibolites can be classified into two groups according to their REE patterns and trace element features. Rocks of the first group are depleted in LREE while rocks of the second group are slightly depleted in LREE or flat from LREE to HREE without significant Eu anomaly. The first group of rocks have (La/Yb)N=0.33-0.55, (La/Sm)N= 0.45-0.65, and their La/Nb, Ce/Zr, Zr/Nb, Zr/Y and Ti/Y ratios are averaged at 1.20, 0.12, 31.02, 2.92 and 198, respectively, close to those of typical N-MORB. The second group of rocks have (La/Yb)N=0.63-0.95, (La/ Sm)N = 0.69--0.90, and their average La/Nb, Ce/Zr, Zr/Nb, Zr/Y and Ti/Y ratios are 0.82, 0.83, 1.15, 0.16, 19.00, 2.58 and 225, respectively, which lie between those of typical N-MORB and E-MORB but closer to the former. The two groups of rocks both exhibit flat patterns from Th to Yb in th 相似文献
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The Shushui Complex can be divided into three rock units based on field investigation, petrography and geochemistry:(1) felsic
gneisses, (2) supracrustal rocks consisting of amphibolite, marble and quartzite, and (3) late granites. Of the complex, felsic
gneisses are dominant and formed in the Late Archaean, which were intruded by a basic dyke with a whole-rock Rb-Sr isochron
age of 2264±219 Ma. The data on rare-earth elements as well as on major and trace elements presented for most of the rock
types making up the complex suggest that (1) basic gneisses were produced by partial melting of mantle peridotite, followed
by fractional crystallization, and (2) felsic gneisses produced by varying degree of melting of a mafic source. The most suitable
tectonic setting to account for the generation of both types would be similar to the underplate setting. 相似文献
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Based on their REE features, stratoid or lenticular amphibolites in the Dabie Complex are di-vided into two types:one is characterized by flat REE distribution patterns and the other by LREE-enrichment. Results of the REE quantitative modeling suggest that the amphibolites were formed from 20% partial melting of garnet lherzolite and 35-56% fractional crystallization of olivine(type TH1) or 14-20% fractional crystallization of olivine and clinopyroxene(type TH2). 相似文献
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W.G.Ernst 《中国地球化学学报》1989,8(2):97-111
New major element data for coexisting minerals and bulk-rock REE analyses,combined with previously obtained petrologic/geologic information,allow comparison of Archean mafic-ultramafic meta-igneous rocks from adjacent portions of northeastern Sino-Korean shield .Isotope data published by previous workers document an Early Archean age of formation for metabasaltic rocks now occurring as mafic amphibolite inclusions in tonalitic gneisses west of Bohai Bay(area).Mafic-ultramafic mineral assemblages developed in tonalitic gneisses west of Bohai Bay(areaA).Mafic-ultramafic mineral assemblages developed in amphibolite facies Archean supracrustals east of Bohai Bay(areaB)are chemically similar ,but pre-existing phase associations have been overprinted by the effects of several later metamorphic events.Non0peridotitic area B protoliths appear to be more magnesian ,averaging-12wt.%MgO(versus-7wt.%for area A),and are slightly less fractionated in REE concentrations relative to chondrites(La-Lu=30-8X versus 37-14X for area A),thus perhaps being more mantle-like than area A metabasaltic analogues.The basaltic-komatiitic series east of Bohai Bay probably represents the most ancient crust of that region,being invaded by Archean tonalities,which were subsequently converted to orthogneisses.These observations are compatible with the hypothesis that ,similar to area A metabasaltic rocks now found as amphibolitic inclusions in orthogneisses,are B mafic supracrustals were formed during Early of Middle Archean time ,prior to widespread isofacial amphibolite facies metamorphism(600-700℃,5-7kb,low αH2O). 相似文献
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东疆哈尔里克造山带中角闪石的特征及其地质意义@赵明@王赐银¥南京大学地球科学系哈尔里,克造山,带角闪,石角闪岩,相温压条件东疆哈尔里克造山带中角闪石的特征及其地质意义赵明王赐银(南京大学地球科学系,南京210093)关键词哈尔里克造山带角闪石角闪岩相温压... 相似文献
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