苏鲁超高压榴辉岩中钾长石的超高压相

[1] 深俯冲陆壳岩石部分熔融与苏鲁超高压榴辉岩中长英质多晶包裹体的形成 [J]. 科学通报 , 2009, (13) : 1826 - 1840

[2] 苏鲁榴辉岩中磷灰石的矿物学和微量元素地球化学 [J]. 岩石学报, 2009, 25 (07) : 1663 - 1677

[3] A perspective view on ultrahigh-pressure metamorphism and continental collision in the Dabie-Sulu orogenic belt[J]. ZHENG YongFei CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.Chinese Science Bulletin. 2008(20)

[4] 山东石岛花岗岩复合岩体的侵位深度与苏鲁超高压变质岩的快速折返机制及动力学效应 [J]. 岩石学报, 2007, (12) : 3171 - 3179

[5] Barite in omphacite-hosted K-feldspar + quartz poly-crystalline aggregates from the Sulu eclogites and its implications [J]. Chinese Science Bulletin, 2007, (21) : 2995 - 3001

[6] 苏鲁榴辉岩钾长石+石英聚合体中重晶石矿物及其意义 [J]. 科学通报 , 2007, (19) : 2312 - 2318

[7] Trace elemental records of short-lived heating during exhumation of the CCSD eclogites[J]. ZONG KeQing1, LIU YongSheng1,2, LIU XiaoMing2 ＆ ZHANG BinHui1 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China;2 State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China.Chinese Science Bulletin. 2007(06)

[8] 中国大陆科学钻探主孔540～600m榴辉岩中赤铁矿-钛铁矿固溶体出溶结构的特征及对榴辉岩折返动力学过程的意义 [J]. 岩石学报, 2006, (07) : 1905 - 1914

[9] V／Sc在CCSD主孔榴辉岩中的系统关系:一种可透视变质作用并指示基性岩浆作用的地球化学工具 [J]. 岩石学报, 2006, (07) : 2051 - 2059

[10] 大陆板片多重性俯冲与折返的动力学模式——苏鲁高压超高压变质地体的折返年龄限定 [J]. 岩石矿物学杂志, 2005, (05) : 357 - 368

[1] 深俯冲陆壳岩石部分熔融与苏鲁超高压榴辉岩中长英质多晶包裹体的形成 [J]. 科学通报 , 2009, (13) : 1826 - 1840

[2] 苏鲁榴辉岩中磷灰石的矿物学和微量元素地球化学 [J]. 岩石学报, 2009, 25 (07) : 1663 - 1677

[3] A perspective view on ultrahigh-pressure metamorphism and continental collision in the Dabie-Sulu orogenic belt[J]. ZHENG YongFei CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.Chinese Science Bulletin. 2008(20)

[4] 山东石岛花岗岩复合岩体的侵位深度与苏鲁超高压变质岩的快速折返机制及动力学效应 [J]. 岩石学报, 2007, (12) : 3171 - 3179

[5] Barite in omphacite-hosted K-feldspar + quartz poly-crystalline aggregates from the Sulu eclogites and its implications [J]. Chinese Science Bulletin, 2007, (21) : 2995 - 3001

[6] 苏鲁榴辉岩钾长石+石英聚合体中重晶石矿物及其意义 [J]. 科学通报 , 2007, (19) : 2312 - 2318

[7] Trace elemental records of short-lived heating during exhumation of the CCSD eclogites[J]. ZONG KeQing1, LIU YongSheng1,2, LIU XiaoMing2 ＆ ZHANG BinHui1 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China;2 State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an 710069, China.Chinese Science Bulletin. 2007(06)

[8] 中国大陆科学钻探主孔540～600m榴辉岩中赤铁矿-钛铁矿固溶体出溶结构的特征及对榴辉岩折返动力学过程的意义 [J]. 岩石学报, 2006, (07) : 1905 - 1914

[9] V／Sc在CCSD主孔榴辉岩中的系统关系:一种可透视变质作用并指示基性岩浆作用的地球化学工具 [J]. 岩石学报, 2006, (07) : 2051 - 2059

[10] 大陆板片多重性俯冲与折返的动力学模式——苏鲁高压超高压变质地体的折返年龄限定 [J]. 岩石矿物学杂志, 2005, (05) : 357 - 368