宁镇地区中生代安基山中酸性侵入岩的地球化学:亏损重稀土和钇的岩浆产生的限制

[1] 底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长玢岩的证据 [J]. 地球化学, 2001, (04) : 353 - 362

[2] Adakite-type sodium-rich rocks in Awulale Mountain of west Tianshan:Significance for the vertical growth of continental crust[J]. XIONG Xiaolin, ZHAO Zhenhua, BAI Zhenghua, MEI Houjun, WANG Yixian, WANG Qiang, XU Jifeng, Niu Hecai ＆ BAO Zhiwei1. Guangzhou Institute of Geochemistry ,Chinese Academy of Sciences, Guangzhou 510640, China;2. State Key Laboratory of Mineral Deposit Research of Nanjing University, Nanjing 210093, China.Chinese Science Bulletin. 2001(10)

[3] 中国东部燕山期埃达克岩的特征及其构造-成矿意义 [J]. 岩石学报, 2001, (02) : 236 - 244

[4] 燕山中晚期的中国东部高原:埃达克岩的启示 [J]. 地质科学, 2001, (02) : 248 - 255

[5] 准噶尔北缘晚古生代岛弧中与俯冲作用有关的adakite火山岩:消减板片部分熔融的产物 [J]. 科学通报 , 2001, (08) : 684 - 688

[6] 一种新的火成岩——埃达克岩的研究综述 [J]. 地球科学进展, 2001, (02) : 201 - 208

[7] 西天山阿吾拉勒adakite型钠质中酸性岩及地壳垂向增生 [J]. 科学通报, 2001, (04) : 281 - 287

[8] The recognition of adakite-type gneisses in the North Dabie Mountain and its implication to ultrahigh pressure metamorphic geology[J]. WANG Qiang, XU Jifeng, WANG Jianxin, ZHAO Zhenhua, WANG Renjing, QIU Jiaxiang, XIONG Xiaolin, SANG Longkang ＆ PENG Lianhong Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;Huhei Regional Geological Survey. Wuhan 430000, China;China University of Geosciences, Wuhan 430074, China Correspondence should be addressed to Wang Q

[9] 宁镇地区花岗岩类岩石谱系单位的初步划分 [J]. 江苏地质, 2000, (02) : 81 - 86

[10] 北大别山adakite型灰色片麻岩的确定及其与超高压变质作用的关系 [J]. 科学通报 , 2000, (10) : 1017 - 1024

[1] 底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长玢岩的证据 [J]. 地球化学, 2001, (04) : 353 - 362

[2] Adakite-type sodium-rich rocks in Awulale Mountain of west Tianshan:Significance for the vertical growth of continental crust[J]. XIONG Xiaolin, ZHAO Zhenhua, BAI Zhenghua, MEI Houjun, WANG Yixian, WANG Qiang, XU Jifeng, Niu Hecai ＆ BAO Zhiwei1. Guangzhou Institute of Geochemistry ,Chinese Academy of Sciences, Guangzhou 510640, China;2. State Key Laboratory of Mineral Deposit Research of Nanjing University, Nanjing 210093, China.Chinese Science Bulletin. 2001(10)

[3] 中国东部燕山期埃达克岩的特征及其构造-成矿意义 [J]. 岩石学报, 2001, (02) : 236 - 244

[4] 燕山中晚期的中国东部高原:埃达克岩的启示 [J]. 地质科学, 2001, (02) : 248 - 255

[5] 准噶尔北缘晚古生代岛弧中与俯冲作用有关的adakite火山岩:消减板片部分熔融的产物 [J]. 科学通报 , 2001, (08) : 684 - 688

[6] 一种新的火成岩——埃达克岩的研究综述 [J]. 地球科学进展, 2001, (02) : 201 - 208

[7] 西天山阿吾拉勒adakite型钠质中酸性岩及地壳垂向增生 [J]. 科学通报, 2001, (04) : 281 - 287

[8] The recognition of adakite-type gneisses in the North Dabie Mountain and its implication to ultrahigh pressure metamorphic geology[J]. WANG Qiang, XU Jifeng, WANG Jianxin, ZHAO Zhenhua, WANG Renjing, QIU Jiaxiang, XIONG Xiaolin, SANG Longkang ＆ PENG Lianhong Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;Huhei Regional Geological Survey. Wuhan 430000, China;China University of Geosciences, Wuhan 430074, China Correspondence should be addressed to Wang Q

[9] 宁镇地区花岗岩类岩石谱系单位的初步划分 [J]. 江苏地质, 2000, (02) : 81 - 86

[10] 北大别山adakite型灰色片麻岩的确定及其与超高压变质作用的关系 [J]. 科学通报 , 2000, (10) : 1017 - 1024