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首页> 外文期刊>Geological Society of America Bulletin >Polyphase tectonothermal history recorded in granulitized gneisses from the north Qaidam HP/UHP metamorphic terrane,western China:Evidence from zircon U-Pb geochronology
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Polyphase tectonothermal history recorded in granulitized gneisses from the north Qaidam HP/UHP metamorphic terrane,western China:Evidence from zircon U-Pb geochronology

机译:中国西部柴达木北部高压/超高压变质地层颗粒状片麻岩中记录的多相构造热历史:锆石U-Pb年代学证据

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High-grade gneisses of the north Qaidam high-pressure/ultrahigh-pressure metamorphic terrane enclose minor eclogites and ultramafic rocks.In combination with pet-rological data,sensitive high-resolution ion microprobe U-Pb geochronology on the granulitized gneisses in the Luliangshan and Xitieshan,western north Qaidam Mountains,reveals a polyphase tectonothermal history including Early Neoproterozoic and Early Paleozoic events.The rocks investigated are two granulite-facies paragneisses and one orthogneiss that both surround garnet peridotite in the Luliangshan,and two paragneisses that enclose eclogite in the Xitieshan.The inherited zircon cores from paragneiss and orthogneiss yield ages between ca.1000 Ma and ca.2500 Ma,representing Mesoproterozoic to Archaean source material for these gneisses.A ca.900 Ma age obtained from one orthogneiss and one paragneiss is interpreted as the age of simultaneous Early Neoproterozoic magmatism and metamorphism.This Early Neoproterozoic tectonothermal event is similar in age to the Jinning orogeny,which is commonly recognized in the metamorphic basement of the south China block,and suggests that the north Qaidam Mountains have an affinity to the south China block.Early Paleozoic metamorphism is recorded in all gneiss samples.In conjunction with cathodoluminescence imagery and mineral inclusions,U-Pb dating of zircons reveals two Early Paleozoic age groups:ca.450 Ma represents the age of high-pressure granulite metamorphism (Grt + Rt inclusions in zircon;kyanite porphyro-blasts),whereas ca.425 Ma reflects the time of medium-pressure,granulite-facies metamorphism (PI + Sil inclusions in zircon) and associated anatexis during decompression.The ages obtained suggest that the granulite-facies metamorphism lasted for ~25 m.y.and was related to the Early Paleozoic continental collision between the Qilian and Qaidam blocks,and to subsequent thermal relaxation and exhumation.
机译:柴达木北部高压/超高压变质地层中的高级片麻岩包裹着少量的榴辉岩和超镁铁质岩石。结合岩石学资料,对吕梁山和吕梁山颗粒状片麻岩进行了高分辨率的高分辨率离子微探针U-Pb地质年代学研究。柴达木山脉西北部的Xitieshan揭示了一个多相构造热历史,包括新元古代和早古生代事件。所研究的岩石是在吕梁山中的两个花岗质岩长石和一个正长片岩都包围着石榴石橄榄岩,以及两个在Xitieshan中包裹着榴辉岩的长石。从帕格尼属和原片麻岩中继承的锆石核的年龄在大约1000 Ma至大约2500 Ma之间,代表了这些片麻岩的中元古代到古生代的原始材料。从一个正片麻片和一个帕格尼属获得的大约900 Ma年龄被解释为该年龄。的新元古代早期岩浆作用和变质作用大型事件的年龄与金宁造山带相似,这在华南地块的变质基底中是公认的现象,并表明柴达木北部与华南地块具有亲合力。所有片麻岩样品都记录了早古生代变质结合阴极发光图像和矿物包裹体,锆石的U-Pb测年揭示了两个早期古生代年龄:约450 Ma代表高压花岗石变质的年龄(锆石中的Grt + Rt包裹体;蓝晶石斑岩爆破),而大约425 Ma反映了减压过程中中压,粒相相变质(锆石中的PI + Sil夹杂物)和相关的厌食时间。获得的年龄表明,粒相相变质持续了约25 myand,与祁连和柴达木块体之间的早古生代大陆碰撞,以及随后的热弛豫和回火。

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