Metamorphic Temperature Investigation of Coexisting Calcite and Dolomite Marble Examples from Nikani Ghar Marble and Nowshera Formation,Peshawar Basin,Pakistan

查看全文 作　　者：Muhammad [1,2]Fahad;Yaseen [2]Iqbal;Mohammad [3]Riaz;Rick [4]Ubic;Simon A. T. [5]Redfern

机构地区：[1]Department of Electrical Engineering, COMSATS Institute of Information Technology, Abbottabad 22010, Pakistan;[2]Materials Research Laboratory, Department of Physics, University of Peshawar, Peshawar 25120, Pakistan;[3]National Centre of Excellence in Geology, University ofPeshawar, Peshawar 25120, Pakistan;[4]College of Engineering Boise State University, Boise 83401, USA;[5]Department of Earth Sciences, University of Cambridge, Cambridge 999020, United Kingdom

出　　处：《Journal of Earth Science》索引2016年第27卷第6期,共9页

基　　金：the financial support extended by the Higher Education Commission (HEC),Pakistan and National Academy of Sciences (USA),project ID 131,under the PAK-USA S & T Cooperation Program,Award (No.0521315);the HEC,Pakistan for their support in the form of “International Research Support Initiative Program (IRSIP)” to conduct a part of research at Department of Earth Sciences,University of Cambridge,UnitedKingdom;financial support extended by the Directorate of S & T,KP regarding minerals upgradation 摘　　要：用从从北巴基斯坦的 Nikani Ghar 云石和 Nowshera 形成的云石样品,变态的温度的决心在方解石白云石 solvus 地温计的帮助下被承担。云石的二种类型,也就是说,方解石白云石大理石和忍受石英的方解石白云石大理石被选择。Petrographic 和白云石样品的扫描电子显微镜分析显示了不同谷物尺寸。X 光检查衍射技术显示了方解石 MgCO ₃ 内容直到 7.93 mol.% 。Nikani Ghar 云石样品从 Nowshera 形成作为与样品相比显示出 MgCO ₃ 的更低的内容。calcite-dolomite-quartz 云石也显示出相对更低的 MgCO ₃ 内容和因此相当低的温度(~ 500 使活跃之物转变生长因素贝它 1 独立,而吗? 关键词：变质温度巴基斯坦白云石方解石大理石大理岩拉形扫描电子显微镜分析

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Metamorphic Temperature Investigation of Coexisting Calcite and Dolomite Marble Examples from Nikani Ghar Marble and Nowshera Formation,Peshawar Basin,Pakistan

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