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Geochronology of the volcanic rocks in the Lu-Zong basin and its significance

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Science China Earth Sciences 2008年第10期51卷 1470-1482页

作者： David COOKE sebastien meffre Centre of Excellence in Ore Deposits (CODES) University of Tasmania

The Lu-Zong (Lujiang-Zongyang) basin is one of the most important volcanic basins in the middle and lower reaches of the Yangtze River area, China. It comprises four shoshonitic volcanic units, which are, in an ascending order, the Longmenyuan, Zhuanqiao, Shuangmiao and Fushan Groups. The LA-ICP MS U-Pb zircon ages of the four units are: 134.8±1.8 Ma for the Longmenyuan Group, 134.1±1.6 Ma for the Zhuanqiao Group, 130.5±0.8 Ma for the Shuangmiao Group, and 127.1±1.2 Ma for the Fushan Group. The results indicate that all volcanic rocks in the Lu-Zong basin were formed in the Early Cretaceous from about 135 Ma to 127 Ma, lasting 8-10 Ma. There were no Jurassic volcanic activities in all the volcanic basins including the Lu-Zong basin in the middle and lower reaches of the Yangtze River area. This work has provided new chronological results for the further study and understanding of the tec- tonic, magmatic and metallogenic processes of eastern China in the Mesozoic.

关键词： zircon LA-ICP MS dating volcanic rocks geochronologic age Lu-Zong basin

Characterization of Galena and Vein Paragenesis in the Penjom Gold Mine,Malaysia:Trace Elements,Lead Isotope Study and Relationship to Gold Mineralization Episodes

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Acta Geologica Sinica(English Edition) 2015年第6期89卷 1914-1925页

作者： Zakaria ENDUT NG Tham Fatt Jasmi Hafiz ABDUL AZIZ sebastien meffre Charles MAKOUNDI Department of Geology Faculty of ScienceUniversity Malaya CODES ARC Centre of Excellence in Ore Deposits University of Tasmania

The Penjom Gold Mine is located 30 km from the Bentong-Raub Suture at the western boundary of the Central Belt in Peninsular Malaysia. Gold mineralization hosted within the vein system is associated with pyrite, arsenopyrite, and minor base metals including galena. Trace element and lead isotope analysis was undertaken on nine samples that represent two stages of galena formed during two tectonic events. Both the Pb isotopes and the trace elements show that the first stage galena within the mineralized areas at the footwall has different geochemical characteristics compared with galena in non mineralized areas in the hanging wall, suggesting that galena crystallized from two different ore fluids and probably at two different times. Higher Te, Se and Bi in the galena from the mineralized area may indicate hydrothermal fluids that migrate through the structural conduit and leached out the metal along the pathway that consist of dominant carbonaceous unit. The Pb isotopic ratio composition are transitional between the bulk crustal growth and an upper crustal growth curve, indicating that derivation was from arc rocks associated with continental crust or a crustal source that includes arc volcanic and old continental sedimentary rocks.

关键词： Vein paragenesis galena trace elements lead isotope and gold mineralization

Linking gold mineralization to regional-scale drivers of mineral systems using in situ U-Pb geochronology and pyrite LA-ICP-MS element mapping

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Geoscience Frontiers 2019年第1期10卷 89-105页

作者： Imogen O.H.Fielding Simon P.Johnson sebastien meffre Jianwei Zi Stephen Sheppard Ross R.Large Birger Rasmusseng Department of Applied Geology Curtin University Geological Survey of Western Australia CODES ARC Centre of Excellence in Ore Deposits University of Tasmania State Key Lab of Geological Processes and Mineral Resources China University of GeosciencesWuhan John de Laeter Centre Curtin University Calidus Resources Ltd School of Earth Sciences The University of Western Australia

Proterozoic orogens commonly host a range of hydrothermal ores that form in diverse tectonic settings at different times. However, the link between mineralization and the regional-scale tectonothermal evolution of orogens is usually not well understood, especially in areas subject to multiple hydrothermal events.Regional-scale drivers for mineral systems vary between the different classes of hydrothermal ore, but all involve an energy source and a fluid pathway to focus mineralizing fluids into the upper crust. The Mount Olympus gold deposit in the Proterozoic Capricorn Orogen of Western Australia, was regarded as an orogenic gold deposit that formed at ca. 1738 Ma during the assembly of Proterozoic Australia. However,the trace element chemistry of the pyrite crystals closely resembles those of the Carlin deposits of Nevada,with rims that display solid solution gold accompanied by elevated As, Cu, Sb, Hg, and Tl, surrounding gold-poor cores. New SHRIMP UeP b dating of xenotime intergrown with auriferous pyrite and ore-stage alteration minerals provided a weighted mean^(207) Pb*/^(206) Pb* date of 1769 ± 5 Ma, interpreted as the age of gold mineralization. This was followed by two discrete episodes of hydrothermal alteration at 1727 ± 7 Ma and 1673 ± 8 Ma. The three ages are linked to multiple reactivation of the crustal-scale Nanjilgardy Fault during repeated episodes of intracratonic reworking. The regional-scale drivers for Carlin-like gold mineralization at Mount Olympus are related to a change in tectonic regime during the final stages of the intracratonic 1820 -1770 Ma Capricorn Orogeny. Our results suggest that substantial sized Carlin-like gold deposits can form in an intracratonic setting during regional-scale crustal reworking.

关键词： Geochronology Xenotime SHRIMP LA-ICP-MS Gold mineralization Capricorn orogen

新疆西准噶尔地区塔斯特岩体锆石LA-ICPMS年龄及其意义

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岩石学报 2007年第8期23卷 1901-1908页

作者：范裕周涛发袁峰谭绿贵 David COOKE sebastien meffre 杨文平何立新合肥工业大学资源与环境工程学院合肥230009 澳大利亚塔斯马尼亚大学优秀矿床研究中心(CODES) 新疆地质勘查局第四地质大队阿勒泰836500

西准噶尔萨吾尔地区地处新疆阿勒泰地区吉木乃县及塔城地区和丰县。酸性侵入岩在区内较发育,其研究对于准噶尔地区后碰撞构造-岩浆演化时限的厘定具有重要的意义。塔斯特岩体是萨吾尔地区重要的复式花岗岩体,与区内铜、金矿化关系密切... 详细信息

西准噶尔萨吾尔地区地处新疆阿勒泰地区吉木乃县及塔城地区和丰县。酸性侵入岩在区内较发育,其研究对于准噶尔地区后碰撞构造-岩浆演化时限的厘定具有重要的意义。塔斯特岩体是萨吾尔地区重要的复式花岗岩体,与区内铜、金矿化关系密切。塔斯特岩体锆石 LA—ICPMS 年龄为337±4Ma(1σ),形成于早石炭世。结合已有的地球化学特征研究,这一年龄显示西准噶尔地区在早石炭世已处于后碰撞环境。本文获得的塔斯特岩体成岩年龄是目前在准噶尔地区获得的最老的后碰撞花岗岩锆石 U—Pb 年龄之一,为准噶尔地区后碰撞构造-岩浆演化时限的厘定提供了新的证据。

关键词：花岗岩塔斯特岩体 LA-ICPMS 后碰撞萨吾尔准噶尔新疆

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东天山自然铜矿化区火山岩的年代学

矿物学报 2007年第Z1期27卷 118-119页

作者：袁峰周涛发范裕谭绿贵 David Cooke sebastien meffre 王庆民王卫江合肥工业大学学艺术资源与环境工程学院安徽合肥230009 澳大利亚塔斯马尼亚大学优秀矿床研究中心(CODES) 霍巴特新疆维吾尔自治区地质调查院新疆乌鲁木齐830000

　　近年来在东天山十里坡、黑龙峰、长城山、东尖峰一带相继发现了与玄武岩有关的自然铜矿化这一新矿化类型(董连慧等,2003),并已有一定程度的研究(崔彬等,2006;袁峰等,2006,2007).关于自然铜的成矿作用,一般认为与溢流玄武岩关系密切... 详细信息

　　近年来在东天山十里坡、黑龙峰、长城山、东尖峰一带相继发现了与玄武岩有关的自然铜矿化这一新矿化类型(董连慧等,2003),并已有一定程度的研究(崔彬等,2006;袁峰等,2006,2007).关于自然铜的成矿作用,一般认为与溢流玄武岩关系密切(朱炳泉,2003;White和Mck-enzie,1995),玄武岩的形成时代、形成机制、岩浆演化等对自然铜的成矿作用有重要的制约(Zhu等,2003;Puschner,2001).本文重点对东天山自然铜矿化区进行火山岩年代学研究.……

关键词：东天山自然铜矿化矿化区火山岩溢流玄武岩成矿作用年代学研究岩浆演化形成时代形成机制矿化类型制约尖峰继发程度长城

安徽庐枞(庐江-枞阳)盆地火山岩的年代学及其意义

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中国科学（D辑） 2008年第11期38卷 1342-1353页

作者：周涛发范裕袁峰陆三明尚世贵 David Cooke sebastien meffre 赵国春合肥工业大学资源与环境工程学院合肥230009 安徽省地质调查与环境中心合肥230001 安徽省地矿局327地质队合肥230011 Centre of Excellence in Ore Deposits(CODES) University of TasmaniaPrivate Bag 79HobartAustralia 香港大学地球科学系中国香港

庐枞盆地是长江中下游地区最重要的火山岩盆地之一,发育有龙门院、砖桥、双庙和浮山4组以橄榄安粗岩系为特征的火山岩地层.通过对4组火山岩中熔岩的锆石LA-ICPMS同位素定年,得到各组火山岩形成的时间分别为:龙门院组(134.8±1.8)Ma、砖... 详细信息

庐枞盆地是长江中下游地区最重要的火山岩盆地之一,发育有龙门院、砖桥、双庙和浮山4组以橄榄安粗岩系为特征的火山岩地层.通过对4组火山岩中熔岩的锆石LA-ICPMS同位素定年,得到各组火山岩形成的时间分别为:龙门院组(134.8±1.8)Ma、砖桥组(134.1±1.6)Ma、双庙组(130.5±0.8)Ma和浮山组(127.1±1.2)Ma.庐枞盆地内火山岩皆形成于早白垩世,火山岩浆活动发生的起止时间约为135～127Ma,持续时间在8～10Ma左右.包括庐枞盆地在内的长江中下游地区各火山岩盆地均不存在侏罗纪火山岩浆活动.研究结果为进一步探讨和认识长江中下游及中国东部中生代构造-岩浆-成矿作用提供了新的年代学成果.

关键词： LA—ICP MS同位素定年火山岩形成时代庐枞盆地

新疆东天山十里坡自然铜矿化区马头滩组玄武岩锆石LA-ICPMS U-Pb年龄及其意义

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岩石学报 2007年第8期23卷 1973-1980页

作者：袁峰周涛发范裕谭绿贵 DavidCOOKE sebastienmeffre 王庆民王卫江合肥工业大学资源与环境工程学院合肥230009 澳大利亚塔斯马尼亚大学优秀矿床研究中心(CODES) 新疆维吾尔自治区地质调查院乌鲁木齐830000

新疆北部东天山十里坡地区近年来新发现了与玄武岩有关的自然铜矿化这一新类型。自然铜的赋矿地层-马头滩组中的赋矿玄武岩锆石 LA-ICPMS 年龄为307±4Ma,对应于晚石炭世,显示该套赋矿地层属于上石炭统。从该区自然铜赋矿火山岩所限定... 详细信息

新疆北部东天山十里坡地区近年来新发现了与玄武岩有关的自然铜矿化这一新类型。自然铜的赋矿地层-马头滩组中的赋矿玄武岩锆石 LA-ICPMS 年龄为307±4Ma,对应于晚石炭世,显示该套赋矿地层属于上石炭统。从该区自然铜赋矿火山岩所限定的时间看,成矿背景应属于后碰撞环境。东天山十里坡地区自然铜矿化的构造背景、成矿系统和矿化类型与峨眉山玄武岩自然铜矿化和美国基威诺铜矿床均存在差异,自然铜矿化的成因可能也存在差异。

关键词：自然铜玄武岩 LA-ICPMS 后碰撞十里坡东天山