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Acta Geologica Sinica(English Edition) 1994年第3期68卷 267-281页

作者： zhuang yuxun Institute of Geology, CAGS, Beijing Chinese Academy of Geological Sciences Beijing

A series of thermal-structural-gneiss domes (briefly TSG domes) are developed in the Chinese Altaides. Sericite-chlorite zone, biotite zone, garnet zone, staurolite zone, kyanite (andalusite)zone, sillimanite- cordierite (sillimanite-garnet)zone, migmatite zone and migmatic granite- gneiss field are developed from the low-grade metamorphic area to the centre of the TSG domes. The succession of the formation and evolution of the progressive metamorphic zone, migmatite zone and migmatic granite-gneiss corresponds to the spatial sequence from the outer part to the centre of the TSG domes. The peak temperature of the metamorphism and granitization increases progressively from 400℃ to 800℃ while the pressure decreases progressively from 1.05 GPa to 0.10 GPa from the biotite zone to the migmatic granite-gneiss field. The metamorphism of the erogenic belt may be described by the pressure-temperature-space-time model (PTst). In the main episode of orogeny, the deep heat flow and structural flow upsurged along a series of the centres of the regional thermodynamic anomalies, giving rise to the progressive metamorphism, granitization, and the differential uplift and the formation of TSG domes.

关键词： Chinese Altaides PTst evolution TSG dome

SHRIMP U-Pb Dating of Zircons of a Dark Eclogite and a Garnet-bearing Gneissic Granitic Rock from Bixiling,Eastern Dabie Area,Anhui Province:Isotope Chronological Evidence of Neoproterozoic UHP Metamorphism

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Acta Geologica Sinica(English Edition) 2000年第4期74卷 748-765页

作者： CHENG Yuqi LIU Dunyi I.S. WILLIAMS JIAN Ping zhuang yuxun GAO Tianshan Institute of Geology Chinese Academy of Geological SciencesBeijing 100037China Research School of Earth Sciences Australian National UniversityAustralia Anhui Geological Survey Hefei 230011AnhuiChina

The paper reports SHRIMP U-Pb zircon data of a dark eclogite and a post-eclogite garnet-bearing gneissic granitic rock from the Bixiling area, Yuexi County, Anhui Province, in the eastern Dabie Mountains. The eclogite, which is metamorphosed basic tuff, contains very scarce zircons in omphacite or garnet, but more zircons in quartz. They usually exhibit a double-layered texture, as shown clearly in cathodoluminescence images. Their inner main parts give a 206Pb/238U age of 757±7 Ma, representing the approximate age of the high-pressure (HP)- ultrahigh-pressure (UHP) metamorphic event during which the eclogite was formed. The outer peripheral parts of the zircons, which have been modified by late-stage fluids, give an age of 223±3 Ma. The granitic rock contains more zircons of anatectic origin found mostly in feldspar and quartz and usually also showing a similar composite texture. The inner main parts of the anatectic zircons with oscillatory zoning give a 206Pb/238U age of 727±15 Ma for the approximate age of the emplacement of the granitic rock, and their outer parts, an age of 219±3 Ma for a similar or even the same fluid event. It is thus suggested that the HP-UHP metamorphism of the Bixiling eclogite facies rocks took place during the Neoproterozoic Jinningian, and the Indosinian age values may only represent a late event in the nature of fluid activity.

关键词： Bixiling dark eclogite garnet-bearing gneissic granitic rock Neoproterozoic Jinningian SHRIMP dating

鲁西孟家屯一种细粒斜长角闪岩的锆石SHRIMP年代学

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地球学报 2005年第5期26卷 429-434页

作者：杜利林庄育勋杨崇辉万渝生王新社中国科学院地质与地球物理研究所中国地质科学院地质研究所北京100037 中国地质调查局北京离子探针中心北京100037

在对鲁西孟家屯地区一种细粒斜长角闪岩变质侵入体的矿物岩相学和锆石微区特征研究的基础上,通过锆石离子探针测定获得了2 604±11Ma的变质作用年龄.结合孟家屯岩组的年龄资料和鲁西地区的岩浆活动时代特征,认为鲁西地区在2.65～2.6 Ga... 详细信息

在对鲁西孟家屯地区一种细粒斜长角闪岩变质侵入体的矿物岩相学和锆石微区特征研究的基础上,通过锆石离子探针测定获得了2 604±11Ma的变质作用年龄.结合孟家屯岩组的年龄资料和鲁西地区的岩浆活动时代特征,认为鲁西地区在2.65～2.6 Ga时期是一个强烈的构造活动时期,与同时期华北地台其他地区的构造活动有很大的差异,具有其独特的地质演化历史.

关键词：鲁西细粒斜长角闪岩年代学华北地台 SHRIMP年代学斜长角闪岩鲁西地区锆石细粒特征研究

大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析——晋宁期高压—超高压变质作用的同位素年代学依据

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地质学报 2000年第3期74卷 193-205页

作者：程裕淇刘敦一 I.S.Williams 简平庄育勋高天山中国地质科学院地质研究所北京100037 National University of Australia G.P.O.Box 4 安徽省地质调查院合肥230026

本文报道大别山安徽省岳西县碧溪岭深色榴辉岩和片麻状花岗质岩石的锆石SHRIMP分析结果。深色榴辉岩的原岩为基性凝灰岩,锆石在岩石中主要产于石英、石榴子石和绿辉石内,为高压一超高压变质作用的产物,内部主体形成年龄约为757±7Ma,代... 详细信息

本文报道大别山安徽省岳西县碧溪岭深色榴辉岩和片麻状花岗质岩石的锆石SHRIMP分析结果。深色榴辉岩的原岩为基性凝灰岩,锆石在岩石中主要产于石英、石榴子石和绿辉石内,为高压一超高压变质作用的产物,内部主体形成年龄约为757±7Ma,代表高压—超高压榴辉岩相变质事件的时代;经受了后期流体改造的锆石边部年龄为223±3Ma。在片麻状花岗质岩石中,发育韵律环带结构的深熔锆石形成于约727±15Ma,受后期流体改造的锆石边部年龄为219±3Ma。综合野外地质关系、区域地质背景和锆石的岩相学特征,笔者提出了碧溪岭榴辉岩相岩石高压—超高压变质作用发生于晋宁期,印支期仅代表一次后期流体改造事件的观点。

关键词：深色榴辉岩片麻状花岗质岩石 SHRIMP测年

鲁西新泰孟家屯2.7Ga变质沉积岩与黑云斜长片麻岩锆石Hf同位素特征

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地质学报 2010年第7期84卷 991-1001页

作者：杜利林杨崇辉庄育勋韦汝征万渝生任留东侯可军中国地质科学院地质研究所北京100037 中国科学院地质与地球物理研究所北京100029 中国地质调查局北京100037 灵宝黄金股份有限公司河南灵宝472500 北京离子探针中心北京100037 中国地质科学院矿产资源研究所国土资源部成矿作用与资源评价重点实验室北京100037

对出露于山东新泰孟家屯2.7Ga的孟家屯岩组中石榴石石英岩(M08)、含十字石石榴石黑云母石英片岩(D242-Y2)和黑云斜长片麻岩(M03)(TTG质片麻岩)进行锆石Lu-Hf同位素分析。石榴石石英岩锆石核部176Lu/177Hf、176Hf/177Hf变化范围为0.00173... 详细信息

对出露于山东新泰孟家屯2.7Ga的孟家屯岩组中石榴石石英岩(M08)、含十字石石榴石黑云母石英片岩(D242-Y2)和黑云斜长片麻岩(M03)(TTG质片麻岩)进行锆石Lu-Hf同位素分析。石榴石石英岩锆石核部176Lu/177Hf、176Hf/177Hf变化范围为0.001730～0.002546、0.281249～0.281360,锆石变质边部176Lu/177Hf、176Hf/177Hf变化范围为0.000123～0.002070、0.281241～0.281318;含十字石石榴石黑云母石英片岩锆石核部176Lu/177Hf、176Hf/177Hf变化范围为0.001334～0.002169、0.281226～0.281324,锆石变质边部176Lu/177Hf、176Hf/177Hf变化范围为0.000445～0.001375、0.281227～0.281309;黑云斜长片麻岩锆石176Lu/177Hf、176Hf/177Hf变化范围为0.000315～0.000847、0.281186～0.281265。孟家屯岩组石榴石英岩、含十字石石榴石黑去母石英片岩中碎屑(岩浆)锆石和黑云斜长片麻岩中岩浆锆石的εHf(t)分别为3.75～7.26、2.31～7.26和3.21～6.27,同时TDM1与其U-Pb年龄非常接近,表明它们起源于新生地壳的部分熔融。结合区域研究资料认为,2.7Ga是鲁西重要的一期构造岩浆热事件,也可能是华北克拉通重要的构造岩浆活动时期。变质沉积岩中许多变质增生锆石相对于核部岩浆锆石低176Lu/177Hf、高176Hf/177Hf,显示变质作用过程中石榴石的存在对锆石的Lu-Hf同位素体系有很大影响。

关键词：孟家屯岩组变质沉积岩黑云斜长片麻岩锆石Hf同位素构造岩浆事件