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TANG Jinhui, LOU Feng, GAN Bingyan, HUANG Wensheng. 2016: LA-ICP-MS zircon U-Pb age of Early Jurassic granite basement in Rencha Volca-nic Basin and its geological significance. Geological Bulletin of China, 35(6): 989-997.
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Rencha basin is one of the typical Mesozoic-Cenozoic volcanic fault basins in northeast Guangdong. Drilling exploration reveals that its basement is mainly composed of Paleozoic metamorphic rocks and graphic granite. In order to further investigate the formation age of the basement rock masses and to improve the knowledge of geological evolution of the area, the authors conducted isotope dating of the samples of graphic granite basement from two drill holes in the basin. The 206Pb/238U measured ages of two groups of zircon by LA-ICP-MS are respectively 179±1Ma and 186Ma, suggesting that the formation age of the graphic granite basement of Rencha Volcanic Basin is late Early Jurassic, i.e., Rencha Basin was formed at the first episode of the Yanshanian mag-matic activity. These ages not only deepen the understanding of the formation and evolution of the Rencha Basin but also provide new chronologic data for the report that northeast Guangdong was lack of magmatic activity in Early Jurassic.
|
宋仕珠, 赵巍, 郑明良, 等.粤东北仁差盆地麻楼逆冲推覆构造特征与铀成矿作用[J].桂林工学院学报, 2010, 26(5):283-287. http://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ201005004.htm
|
|
李文达, 毛建仁, 朱云鹤.中国东南部中生代火成岩与矿床[M].北京:科学出版社, 1998.
|
|
徐先兵, 张岳桥, 贾东, 等.锆石LA-ICP-MS U-Pb与白云母40Ar/39Ar年代学及其对中国东南部早燕山事件的制约[J].地质科技情报, 2010, 29(3):87-94. http://www.doc88.com/p-7478223707902.html
|
|
刘延勇, 卢映新, 梁业武, 等.粤东北仁差盆地火山岩基本特征[J].桂林工学院学报, 2007, 27(2):159-164. http://www.cnki.com.cn/Article/CJFDTOTAL-GLGX200702002.htm
|
|
Liu Y S, Hu Z C, Gao S, et al. In situ analysis of major and trace ele-ments of anhydrous minerals by LA-ICP-MS without applying an internal standard[J].Chemical Geology, 2008,257:34-43. doi: 10.1016/j.chemgeo.2008.08.004
Liu Y S, Hu Z C, Gao S, et al. In situ analysis of major and trace ele-ments of anhydrous minerals by LA-ICP-MS without applying an internal standard[J].Chemical Geology, 2008, 257:34-43. doi: 10.1016/j.chemgeo.2008.08.004
|
|
Liu Y, Gao S, Hu Z, et al.Continental and oceanic crust recyclinginduced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010,51:537-571. doi: 10.1093/petrology/egp082
Liu Y, Gao S, Hu Z, et al.Continental and oceanic crust recyclinginduced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51:537-571. doi: 10.1093/petrology/egp082
|
|
Liu Y, Hu Z, Zong K,et al.Reappraisement and refinement of zir-con U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010,20:1535-1546. http://cn.bing.com/academic/profile?id=2085347045&encoded=0&v=paper_preview&mkt=zh-cn
Liu Y, Hu Z, Zong K, et al.Reappraisement and refinement of zir-con U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 20:1535-1546. http://cn.bing.com/academic/profile?id=2085347045&encoded=0&v=paper_preview&mkt=zh-cn
|
|
Wiedenbeck M, Alle P, Corfu F, et al. Three natural zircon stan-dards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards and Geoanalytical Research, 1995,19:1-23. http://cn.bing.com/academic/profile?id=2039872199&encoded=0&v=paper_preview&mkt=zh-cn
Wiedenbeck M, Alle P, Corfu F, et al. Three natural zircon stan-dards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards and Geoanalytical Research, 1995, 19:1-23. http://cn.bing.com/academic/profile?id=2039872199&encoded=0&v=paper_preview&mkt=zh-cn
|
|
Sláma J, Kosler J, Condon D J, et al. Plesovice zircon_A new natu-ral reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 2008, 249:1235. http://cn.bing.com/academic/profile?id=2169766597&encoded=0&v=paper_preview&mkt=zh-cn
Sláma J, Kosler J, Condon D J, et al. Plesovice zircon_A new natu-ral reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 2008, 249:1235. http://cn.bing.com/academic/profile?id=2169766597&encoded=0&v=paper_preview&mkt=zh-cn
|
|
Ludwig K R. ISOPLOT 3.00:A Geochronological Toolkit for Mi-crosoft Excel[M]. Berkeley:Berkeley Geochronology Center, Cali-fornia,2003.
Ludwig K R. ISOPLOT 3.00:A Geochronological Toolkit for Mi-crosoft Excel[M]. Berkeley:Berkeley Geochronology Center, Cali-fornia, 2003.
|
|
Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002,192:59-79 doi: 10.1016/S0009-2541(02)00195-X
Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192:59-79 doi: 10.1016/S0009-2541(02)00195-X
|
|
Liang H Y, Campbell I H, Allen C M, et al. Zircon Ce4+/Ce3+ ra-tios and ages for Yulong ore-bearing porphyries in eastern Tibet[J]. Miner. Deposit, 2006, 41:152-159. doi: 10.1007/s00126-005-0047-1
Liang H Y, Campbell I H, Allen C M, et al. Zircon Ce4+/Ce3+ ra-tios and ages for Yulong ore-bearing porphyries in eastern Tibet[J]. Miner. Deposit, 2006, 41:152-159. doi: 10.1007/s00126-005-0047-1
|
|
Harris C A, Allen C M, Bryan S E, et al. LA-ICP-MS U-Pb zir-con geochronology of regional volcanism hosting the Bajo de la Alumbrera Cu-Au deposit:Implications for porphyry-related min-eralization[J]. Miner. Deposit, 2004, 39:46-67. doi: 10.1007/s00126-003-0381-0
Harris C A, Allen C M, Bryan S E, et al. LA-ICP-MS U-Pb zir-con geochronology of regional volcanism hosting the Bajo de la Alumbrera Cu-Au deposit:Implications for porphyry-related min-eralization[J]. Miner. Deposit, 2004, 39:46-67. doi: 10.1007/s00126-003-0381-0
|
|
吴元保, 郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报, 2004, 49(16):1589-1604. http://mall.cnki.net/magazine/article/kxtb200416001.htm
|
|
舒良树, 周新民.中国东南部晚中生代构造作用[J].地质论评, 2002, 48(3):249-260 http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200203004.htm
|
|
陈培荣, 华仁民, 章邦桐, 等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学(D辑), 2002, 32(4):279-289. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200204002.htm
|
|
余心起, 狄永军, 吴淦国郑, 等.粤北存在早侏罗世的岩浆活动——来自霞岚杂岩SHRIMP锆石U-Pb年代学的证据[J].中国科学(D辑), 2009, 39(6):681-693. http://www.cqvip.com/main/detail.aspx?id=30743507
|
|
陈培荣, 孔兴功, 倪琦生, 等.赣南燕山早期双峰式火山岩的厘定和意义[J].地质论评, 1999, 45(增刊):734-741. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1999S1105.htm
|
|
许美辉.福建永定地区早侏罗世双峰式火山岩及其构造环境[J].福建地质, 1992, 2:115-125. http://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ199202005.htm
|
|
周金城, 陈荣.闽东南晚中生代壳慢作用地球化学[J].地球化学, 2001, 30(6):547-558 http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200106006.htm
|
|
Li Z X, Li X H. Formation of the 130km-wide intra-continental orogen and post-orogenic magmatic province in Mesozoic South China:A flat-slab subduction model[J]. Geology, 2007,35:179-182. doi: 10.1130/G23193A.1
Li Z X, Li X H. Formation of the 130km-wide intra-continental orogen and post-orogenic magmatic province in Mesozoic South China:A flat-slab subduction model[J]. Geology, 2007, 35:179-182. doi: 10.1130/G23193A.1
|
|
丁兴, 陈培荣, 陈卫锋, 等.湖南沩山花岗岩中锆石LAICPMS UPb定年:成岩启示及意义[J].中国科学(D辑), 2005, 35(7):606-616. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200507001.htm
|
|
邢光福, 杨祝良, 毛建仁, 等.东南大陆边缘早侏罗世火成岩特征及其构造意义[J].地质通报, 2002, 21(7):384-391. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200207004.htm
|
|
王德滋, 周新民.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化[M].北京:科学出版社, 2002:217-229.
|
|
赵希林, 毛建仁, 陈荣, 等.闽西南地区紫金山岩体锆石SHRIMP定年及其地质意义[J].中国地质, 2008, 35(4):590-597. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200804004.htm
|
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