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| 1 | The recognizing of ca. 1.95 Ga tectono-thermal eventin Kong-ling nucleus and its significance for the evolution of Yangtze Block, South China显示文摘Some 1.95 Ga metamorphism of high-grade Ar-chean rocks in Kongling terrain, continental nucleus of Yangtze Block, South China, are recognized by Sm-Nd dating. This event is further confirmed by the ages of single zircon SHRIMP U-Pb and K-Ar analyses of TTG and (or) paragneisses, and intrusions of potassic-granitic batholith in the region. The coincidence in period between the high-grade metamorphism in the Kongling area and the creation of major basement rocks of its neighborhoods of the Yangtze Block around the Kongling Archean nucleus makes it a favorable explanation for their tectonic connections that, in the whole Yangtze Block there was some tectono-thermal event of ca. 2.0-1.8 Ga, which resulted in the formation of unitive Yangtze basement. | LING Wenli GAO Shan ZHANG Benren ZHOU Lian XU Qidong | 2001 | Chinese Science Bulletin2001，46，4： | 29 |
| 2 | U-Pb zircon age of the foliated garnet-bearing granites in western Dabie Mountains,Central China显示文摘U-Pb zircon dating on two foliated garnet-bearing granite samples in the western Dabie ultra-high-pressure (UHP) metamorphic unit yields concordant ages of (234±4) Ma and (227±5) Ma, respectively. These ages, following the UHP peak metamorphism, represent the magma emplacement ages for the foliated garnet-bearing granites. This, for the first time, shows that there are the Triassic granites in the Dabie Mountains. The foliated garnet-bearing granites resemble A-type granite in geochemical characteristics, indicating that they were formed in exten-sional geodynamic setting. The magma formation reflects a reheating event in the Dabie orogenic belt and it enhances the transfer of tectonic regime from collision into extension and promotes the rapid exhumation into lower crust for the UHP metamorphic rocks. | ZHANG Hongfei ZHONG Zengqiu GAO Shan ZHANG Benren LI Huiming | 2001 | Chinese Science Bulletin2001，46，19： | 25 |
| 3 | Pb isotopic geochemical study on the crustal structure of Tongbaishan显示文摘Pb isotopic composition of the Tongbai complex, distributed in the Tongbaishan to the west of the Dabieshan, ranges between the Dabie core complex and the Dabie ultral-high pressure (UHP) metamorphic complex, the latter having more radiogenic Pb isotopic composition than the former. Granites from the Jigongshan pluton, which intruded mainly into the Tongbai complex, are distinct from the Tongbai complex but similar to the Dabie core complex in Pb isotopic composition, showing that the magma of the Jigongshan granites was derived from the partial melting of the Dabie core complex. According to Pb isotopic compositional variation model in the vertical crustal section and magma source from the Jigongshan pluton, it is suggested that the Tongbai complex was an upper rock serial of the Dabie core complex, which is beneath the Dabie UHP metamorphic complex in the crustal structure of the Tongbai-Dabie orogenic belt. The Tongbai complex was not well preserved in the Dabie area due to the high exhumed crustal section. However, the crustal section in the Tongbai area was exhumed less than that in the Dabie area, and the deep crust in the Tongbai area still contains the basement composition similar to the Dabie core complex. Therefore, the crustal basements from the Dabie to Tongbai areas are united. The present distribution of the basement blocks in different locations of the Tongbai-Dabie orogenic belt reflects different exposure of the crustal section. | ZHANG Hongfei, ZHANG Benren, ZHONG Zenqiu, SOU Shutian, ZHANG Haizu and WANG Linsen(China University of Geosciences, Wuhan 430074, China) | 2003 | Progress in Natural Science:Materials International2003，13，1： | 10 |
| 4 | Recognition of Ophiolite Belt and Granulite in Northern Area of Mian-Lue, Southern Qinling, China and Their Implication显示文摘RecognitionofOphioliteBeltandGranuliteinNorthernAreaofMian-Lue,SouthernQinling,ChinaandTheirImplication￥XuJifeng(Departmentof... | Xu Jifeng(Department of Geology, China University of Geosciences, Wuhan 430074)Zhang Benren Han Yinwen(Department of Geochehastry, China University of Geosciences, Wuhan 430074) | 1994 | Journal of Earth Science1994，13，1： | 9 |
| 5 | Discovery of the highly depleted N-MORB-type volcanic rocks: new evidence for the Mianlue paleo-ocean显示文摘The highly depleted N-MORB-type volcanic rocks have been discovered in Mianlue mélange of Qinling orogenic belt, central China. These mafic rocks are associated with the meta-peridotites, showing LREE-depleted pattern, similar to N-MORB and typical ophiolites. It is indicated that an ancient ocean existed in the Mianlue area of Qinling orogenic belt during the late Paleozoic. | Jifeng Xu Xueyuan Yu Xianhua Li Yinwen Han Jihu Shen Benren Zhang | 1998 | Chinese Science Bulletin1998，43，6： | 7 |
| 6 | Geochemistry of Gneisses from Dabie Complex and Tongbai Complex in Qinling-Tongbai-Dabie Orogenic Belt:Implications for Location of Yangtze-Sino-Korean Suture显示文摘The Dabie complex (DC) and the Tongbai complex (TBC) are separately distributed in the middle and eastern parts of the Qinling-Tongbai-Dabie orogenic belt. In this study, the Dabie complex can be divided into two units: one is the complex with no high pressure and ultrahigh pressure metamorphic rocks (DC1), and the other is the complex containing coesite-bearing eclogite lenses or boudins (DC2). Gneisses are predominant in the TBC, DC1 and DC2. Major and trace element data of gneisses in the TBC, DC1 and DC2 show them to be the orthogneisses. The gneisses in the DC1 have higher incompatible element contents and higher ratios of w(K 2O)/w(Na 2O) and w(La) n/w(Yb) n than those in the DC2. However, no obvious differences arise in other element contents and the ratios of w(La)/ w(Nb), w(Nb)/w(Th), w(Nb)/w(Hf), w(Ba)/w(La), w(Sm)/w(Nd) and w(Th)/w(U) between the gneisses in the DC2 and those in the DC1. These observations suggest that the protoliths of the gneisses in the DC2 have affinities to those in the DC1. The difference between the DC1 and DC2 gneisses in incompatible element contents could reflect the difference in their partial melting extent. The TBC gneisses are geochemically similar to the DC1 gneisses, suggesting that the TBC and DC1 gneisses are the same lithologic unit in the Qinling-Tongbai-Dabie orogenic belt and that they have experienced similar formations and evolution histories. In the Qinling-Tongbai area, the TBC is part of the northern blocks of the Yangtze craton. Given the similarity of geochemical characteristics, the rock assemblage and the ages between the TBC and DC1 gneisses, we can infer that the Dabie complex also belongs to the northern blocks of the Yangtze craton. In terms of the distribution of eclogites and metamorphic facies, we propose that the collisional suture in the Dabie area is distributed along the Xiaotian-Mozitan fault, at the contact with the Shang-Dan-Tongbai fault to the west. | Zhang Hongfei Zhang Benren Zhong Zengqiu Gao Shan Hu Shenghong Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074 | 2000 | Journal of Earth Science2000，19，4： | 5 |
| 7 | Pb Isotope Mapping in the Tongbai-Dabie Orogenic Belt, Central China显示文摘摘要:在华中的 Tongbai-Dabie orogenic 带是在 Yangtze 和诺思中国 cratons 之间的 collisional 带的部分。它代表之一最广泛超离频压力(UHP ) 并且高压(HP ) 在世界上的变形岩石。在这个区域印射的 Pb 同位素是一个重要方法抑制外壳的结构和构造进化并且在垂直的构造的栈以内识别构造边界。把 Dabie 的作文基于 Pb 同位素建筑群( DBC ), Tongbai 建筑群( TBC ), UHP 和 HP 变形岩石和联系 foliated 花岗石,从北方 Huaiyang ( NHY )的更低的变形岩石在 Tongbai-Dabie orogenic 的构造的带,和白垩纪花岗石系上带子,我们决定了 Tongbai-Dabie orogenic 带的 Pb 同位素 geochemical 地图。Pb 同位素作文在每地质的身体或 lithotectonic 单位以内是类似的 Pb 同位素地图表演,而是不同 lithotectonic 单位的 Pb 同位素作文在 Tongbai-Dabie orogenic 带显示出系统的变化。NHY 构造的带在 Pb 同位素作文与 Tongbai-Dabie UHP-HP 变形的带强烈形成对照。沿着 Xiaotian-Mozitan 的线指责,这被建议, Tongbai-Dabie UHP 和 HP 的北方限制变形岩石,代表一条重要构造边界。在 Tongbai-Dabie HP-UHP 变形的带以内,到 Xiaotian-Mozitan 差错的南方,以在不同主要 lithotectonic 单位之中的不同 lithotectonic 单位和空间关系的 Pb 同位素作文的垂直变化被抑制了。 | ZHANG Li ZHONG Zengqiu WANG Linsen Zhang Benren | 2008 | Acta Geologica Sinica(English Edition)2008，82，1： | 3 |
| 8 | Geochemical Characteristics of Pb Isotope of High-Pressure Metamorphic Rocks and Foliated Granites from HP Unit of Tongbai-Dabie Orogenic Belt显示文摘Whole-rock Pb isotopic compositions of the high-pressure (HP) metamorphic rocks, consisting of two-mica albite gneisses and eclogites, and foliated granites from the HP metamorphic unit of the Tongbai-Dabie orogenic belt are firstly reported in this paper. The results show that the HP metamorphic rocks in different parts of this orogenic belt have similar Pb isotopic compositions. The two- mica albite gneisses have 206 Pb/ 204 Pb=17.657-18.168, 207 Pb/ 204 Pb=15.318-15.573, 208 Pb/ 204 Pb=38.315-38.990, and the eclogites have 206 Pb/ 204 Pb=17.599-18.310, 207 Pb/ 204 Pb=15.465- 15.615 , 208 Pb/ 204 Pb=37.968-39.143. The HP metamorphic rocks are characterized by upper crustal Pb isotopic composition. Although the Pb isotopic composition of the HP metamorphic rocks partly overlaps that of the ultrahigh-pressure (UHP) metamorphic rocks, as a whole, the former is higher than the latter. The high radiogenic Pb isotopic composition for the HP metamorphic rocks confirms that the subducted Yangtze continental crust in the Tongbai-Dabie orogenic belt has the chemical structure of increasing radiogenic Pb isotopic composition from lower crust to upper crust. The foliated granites, intruded in the HP metamorphic rocks post the HP/UHP metamorphism, have 206 Pb/ 204 Pb=17.128-17.434, 207 Pb/ 204 Pb=15.313-15.422 and 208 Pb/ 204 Pb=37.631-38.122, which are obviously different from the Pb isotopic compositions of the HP metamorphic rocks but similar to those of the UHP metamorphic rocks and the foliated garnet-bearing granites in the UHP unit. This shows that the foliated granites from the HP and UHP units have common magma source. Combined with the foliated granites having the geochemical characteristics of A-type granites, it is suggested that the magma for the foliated granites in the UHP and HP unit would be derived from the partial melting of the retrometamorphosed UHP metamorphic rocks exhumed into middle to lower crust, and partial magmas were intruded into the HP unit. | Zhang Li Zhang Hongfei Zhong Zengqiu Zhang Benren Wang Linsen Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074 | 2003 | Journal of China University of Geosciences2003，14，4： | 3 |
| 9 | Tectonic affinity of Paleozoic stratigraphic slices along the northern margin in Dabie Orogen,central China: evidence from Pb isotope of rocks显示文摘Metavolcanic and metasedimentary rocks from the Paleozoic tectono-stratigraphic units along the northern margin in the Dabie orogen show that there are two types of Pb isotopic compositions, which have some affined regularity with tectonic subdivision. Compared with the main tectonic units of the Qinling orogen, the Dingyuan Formation should be the part of the South Qinling orogenic belt or the northern margin of the Yangtze craton, characterized by less radiogenic Pb isotopic composition, and the Guishan Formation, Nanwan Formation-Foziling Group and the Carboniferous should be the part of the North Qinling orogenic belt which is extended to the east, characterized by more radiogenic Pb isotopic composition. These facts combined with the distribution of the geological units suggest that the Paleozoic subduction zone between the Yangtze and North China cratons should be located in the north boundary of the Nanwan Formation-Foziling Group or somewhere that is covered by the Nanwan Formation-Foziling Group now. From the Pb isotopic evidence and suggestion presented here, one aspect of the constraint is provided for determining the position of the Triassic collision suture between the two cratons. | XU Qidong, OUYANG Jianping, ZHANG Benren and KUANG Shaoping(1. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China 2. Institute of Geochemistry, China University of Geosciences, Wuhan 430074, China) | 2002 | Progress in Natural Science:Materials International2002，12，6： | 3 |
| 10 | Chemical composition of the continental crust as revealed by studies in East China显示文摘 | Gao Shan Luo Tingchuan Zhang Benren Zhang Hongfei Han Yinwen Zhao Zidan Yiken | 1998 | Geochim Cosmochim Acta1998，62，11： | 1 |
| 11 | Neoproterozoic tec- tonic evolution of the northwestern Yangtze craton, South China:implications for amalgamation and break-up of the Rodinia Super- continent显示文摘 | Ling Wen]i Gao Shan Zhang Benren | 2003 | Precambrian Research2003，122，： | 1 |
| 12 | An ECCM model and the technical development trends to the demands of the future EW combat显示文摘 | Benren T | 1994 | IEEE AES Systems Magazine1994，9，6： | 1 |
| 13 | Chemical composition of the continental crust as revealed by studies in East China显示文摘 | Shan Gao Tingchuan Luo Benren Zhang | 1998 | GCA1998，，： | 1 |
| 14 | Neoproterozoic tec-tonic evolution of the northwestern Yangtze craton, South China:implications for amalgamation and break-up of the Rodinia Super-continent显示文摘 | LingWenli Gao Shan Zhang Benren | 2003 | Precambrian Research2003，22，： | 1 |
| 15 | Neoproterozoic tectonic evolution of the northwestern Yangtze craton, South China: Implications for amalgamation and break-up of the Rodinia Supercontinent显示文摘 | LING Wenli GAO Shan ZHANG Benren | 2003 | Precambrian Research2003，122，： | 1 |
| 16 | Neoproterozoic tectonic evolution of the northwestern Yangtze Craton,South China:implications for amalgamation and break-up of the Rodinia Supercontinent显示文摘 | Ling Wenli Gao Shan Zhang Benren | | 0，，： | 1 |
| 17 | An ECCM model technical development trends to the demands of the future EW combat显示文摘 | Benren Tao | 1994 | IEEE AES Systems Magazine1994，9，6： | 1 |
| 18 | An ECCM model and the technical development trends to the demands of the futureEW combat显示文摘 | Benren T | | IEEEAero space and Electronic' Systems Maga zin e0，9，6： | 1 |
| 19 | Chemical composition of the continental crust as revealed by studies in Eastern China 显示文摘 | Gao Shah Luo Tingchuan Zhang Benren | 1998 | Geochinica et Cosmochimica Acta1998，62，11： | 1 |
| 20 | An ECCM model and the technical development trends to the demands of the future EW combat 显示文摘 | Benren T | 1994 | IEEE Aerospace and Electronic Systems Magazine1994，9，6： | 1 |
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