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| 1 | Zircon SHRIMP Dating for the Weiya Pluton, Eastern Tianshan: Its Geological Implications显示文摘The timing of the emplacement of the Weiya pluton remains controversial due to the absence of systematic and precise dating. This paper reports zircon SHRIMP U-Pb dating of different lithologic phases in the Weiya pluton, and discusses the genesis and tectonic environment. The ages of gabbro, quartz syenite, diorite porphyrite and fine-grained granite are 236?6 Ma, 246?6 Ma, 233?8 Ma and 237?8 Ma, respectively. All these phases were formed in early-middle Indosinian (Triassic) in a post-orogenic environment. In addition to underplating, intraplating of mantle-derived magmas is also a substantial mechanism for magma generation and vertical accretion of the continental crust. Granitoid rocks are important products of vertical continental accretion as underplating evolves gradually to intraplating. The existence of post-orogenic Indosinian granites shows that the middle Tianshan orogenic belt underwent an important tectonic conversion from the Paleo-Asian ocean subduction-collision system to the Paleo-Tethys ocean regime. | ZHANG Zunzhong GU Lianxing WU Changzhi LI Weiqiang XI Aihua WANG Shuo | 2005 | Acta Geologica Sinica(English Edition)2005，79，4： | 53 |
| 2 | Pre-collision Granites and Post-collision Intrusive Assemblage of the Kelameili-Harlik Orogenic Belt显示文摘The main types of intrusive rocks in the Kelameili-Harlik Hercynian erogenic belt include calc-alkaline granites, diabase dykes, kaligranites and alkaline granites. Investigation in field geology, petrology, mineralogy and geochemistry shows that the calc-alkaline granites belong to the syntexis-type (or I-type) and were formed in a pre-collisional magmatic arc environment. In consideration of the fact that kaligranites have many features of alkaline granites with higher consolidation temperatures than the calc-alkaline granites and show a discontinuity of minor element and REE evolution in respect to the calc-alkaline granites, they could not have been derived by differentiation of magmas for the calc-alkaline granites, but are likely to have been generated in an environment analogous to that for alkaline granites. The triplet of basic dyke swarms, kaligranites and alkaline granites could be regarded as a prominent indication of the initial stage of post-collisional delamination and extension. These | GU Lianxing HU Shouxi CHU Qiang YU Chunshui XIAO Xinjian | 1999 | Acta Geologica Sinica(English Edition)1999，73，3： | 33 |
| 3 | Advances in research of sulphide ore textures and their implications for ore genesis显示文摘在硫醚矿石质地在的研究的重要进展恨年加深了我们相关矿藏的矿石开始的理解。硫醚矿物质的压力答案为矿石材料的动员作为机制被建议了,而脉石的压力答案被相信提起主要矿石的等级。我们知道了从液体的贱金属硫醚的降水比较喜欢水晶和黄铁矿的裂缝表面形成增生。因此,在一个沉积序列的忍受黄铁矿的胚胎床能作为有效水晶种子床被扮演并且为套印形成巨大的 statabound 沉积物的液体是赞成的。各种各样的硫醚的质地研究能被用来解释矿石的沉积,成岩作用,变丑和变态的全部历史。在闪锌矿的黄铜矿疾病的学习引起了地区精制的想法,并且在巨大的硫醚沉积物把新解释给金属带状配列。硫醚矿石的可锻的砍可以形成矿石糜棱岩,它将成为在套印的迟了阶段的液体期间在 Cu, Au 和 Ag 充实的矿石射击。尽管有那,各种各样的现代分析技术很快正在被开发,是为矿石地质学家的一个 unreplaceable 工具的矿石显微镜学遗体。与这些现代技术结合了,这个工具将帮助在矿石开始上加速理论的发展。 | GU Lianxing ZHENG Yuanchuan TANG Xiaoqian WU Changzhi HU Wenxuan | 2006 | Progress in Natural Science:Materials International2006，16，10： | 15 |
| 4 | Early Indosinian Weiya Gabbro in Eastern Tianshan, China: Elemental and Sr-Nd-O Isotopic Geochemistry, and Its Tectonic Implications显示文摘在东方 Tianshan 的 Weiya 斑粝岩在早 Indosinian.This 期间被形成与 Ce/Pb ( 5.74-10.16 )的低比率,岩石被丰富显著地在大离子亲石元素( LILE )描绘,例如 Rb , K , Ba 和 Pb ,并且在高度回答力量元素( HSFE )例如 U 和 Th ,但是在 Nb 和 Ta 的弄空。Weiya 斑粝岩的所有样品在 LREE (72.58-135.61ppm ) 与中等丰富显示类似的使球粒状陨石正常化的模式,在 HREE (15.26-25.31ppm ) 的中等弄空和在 LREE 和 HREE (L/ H=4.09-5.98 ) 之间的温和分别。岩石的平均起始的 Sr 价值是 0.7069,并且岩石的δ ^(18 ) O 价值变化 from5.67per thousand-8.04per 千。以 Nd 同位素比, Weiya 斑粝岩被(t) 珍视的积极ε _(Nd )(0.52-0.76 ) 描绘。所有这些特征显示 Weiya 斑粝岩的源地是由免除潜水艇 ducted 幼仔大陆地壳的液体的 metasomatized,与有限外壳的污染在岩浆期间上升并且炮兵阵地。大陆人(A 类型) 俯冲被导致由向北方 Paleo-Tethyan 海洋的板的俯冲在期间最近对二叠三叠纪。从这个观点,它被建议那构造变换从对 Paleo-Tethys 政体 thePaleo 亚洲发生了在期间最近二叠或最早三叠纪。 | ZHANG Zunzhong GU Lianxing WU Changzhi | 2007 | Acta Geologica Sinica(English Edition)2007，81，3： | 7 |
| 5 | Oxygen Isotope Characteristics of the Footwall Alteration Zones in the Hongtoushan Volcanogenic Massive Sulfide Deposit,Liaoning Province,China and Restoration of Their Formation Temperatures显示文摘Hongtoushan Volcanogenic 巨大的硫醚存款(VMSD ) 发生在 Hunbei 花岗石绿岩岩层,辽宁省, NE 中国。在采矿区域的岩石在以前的调查在在 600posit 之间的温度在 3.02.8 Ga 附近被变形了到上面的角闪岩外形因为矿石身体在正直的褶层的过渡地点和谐地发生。Re 和 O 为有从矿石身体的闪锌矿和方铅矿的 paragenetic 黄铁矿的同位素的分析被用来决定预定矿化作用并且跟踪 metallogenic 材料的来源。四个黄铁矿的 ReOs 同位素的数据取样构造 isochron,产出 226 攠敮杲敩 ? 景映牯慭楴湯漠 ? 桴 ? 牴癩污湥 ? 慣楴湯 ? 牡 ?湫睯n 的加权的平均年龄吗? | ZHENG Yuanchuan GU Lianxing TANG Xiaoqian LIU Sihai WU Changzhi LI Chunhai | 2011 | Acta Geologica Sinica(English Edition)2011，85，3： | 2 |
| 6 | Geology and genesis of the Upper Paleozoic massive sulphide deposits in South China显示文摘 | Gu Lianxing Hu Wenxuan He Jinxiang | 1993 | Transactions of the Institution of Mining and Metallurgy Section B:Applied earth science1993，，： | 1 |
| 7 | Copper, gold and silver enrichment in ore mylonites within massive sulphide orebodies at Hongtoushan VHMS deposit, NE China显示文摘 | GU Lianxing ZHENG Yuanchuan TANG Xiaoqian | 2007 | Ore Geology Reviews2007，30，1： | 1 |
| 8 | Copper, Gold and Silver Enrichment in Ore Mylonites within Massive Sulphide Orebodies at Hongtoushan, NE China 显示文摘 | Gu Lianxing Zheng Yuanchuan Tang Xiaoqian | 2007 | Ore Geology Reviews2007，30，： | 1 |
| 9 | Copper, Gold and Silver Enrichment in Ore Mylonites Within Massive Sulphide Orebodies at Hongtoushan VHMS Deposit, NE China显示文摘 | Gu Lianxing Zheng Yuanchuan Tang Xiaoqian | 2007 | Ore Geology Reviews2007，30，： | 1 |
| 10 | Multi-episode fluid boiling in the Shizishan copper-gold deposit at Tongling, Anhui Province: its bearing on ore formation显示文摘 | Xinjian Xiao Lianxing Gu Pei Ni | 2002 | Science in China Series D: Earth Sciences2002，，1： | 1 |
| 11 | Formation mechanisms of hydrocarbon reservoirs assoeiated with volcanic and subvolcanic intrusive rocks: Examples in Mesozoic-Cenozoic ba- sins of eastern China 显示文摘 | Wu Changzhi Gu Lianxing Zhang Zunzhong | 2006 | AAPG Bulletin2006，90，1： | 1 |
| 12 | Regional variations in ore composition and fluid features of massive sulfide deposits in South China: Implications for genetic modeling显示文摘 | GU Lianxing HU Wenxuan HE Jinxiang | 2000 | Episodes2000，23，2： | 1 |
| 13 | Rubidium strontium and Lead isotope geology of the Luojiahe granodiorite in the Zhongtiaoshan显示文摘 | Gu Lianxing Liu Xianhua Zhen Yunqing | 1993 | Journal of Nanjing University1993，29，4： | 1 |
| 14 | Formation mechanisms of hydrocarbon reservoirs associat- ed with volcanic and subvolcanic intrusive rocks:examples in Mesozoic - Cenozoic basins of eastern China显示文摘 | WU Changzhi GU Lianxing ZHANG Zunzhong | 2006 | AAPG Bulletin2006，90，1： | 1 |
| 15 | Regional variations in ore composition and fluid features of massive sulphide deposits in South China:Implications for genetic modelling显示文摘 | Gu Lianxing Hu Wenxuan He Jinxiang | 2000 | Episodes2000，23，2： | 1 |
| 16 | Hydrarn reselvoirs in a trachyie porphy intrusion in ihe Fxienl de- pression of tile I Jaohe Basin, norlheast China 显示文摘 | Gu Lianxing Ren Zuowei Wu Changzhi | 2002 | AAPG Bul- letin2002，86，10： | 1 |
| 17 | Formation mechanisms of hydrocarbon reservoirs associated with volcanic and subvolcanic intrusive rocks: Examples in Mesozoic -Cenozoic basin of eastern China 显示文摘 | Wu Changzhi Gu Lianxing | 2006 | AAPG Bulletin2006，90，1： | 1 |
| 18 | Intergrowth of hexagonal and monoclinic pyrrhotites in some sulphide ores from Norway显示文摘 | Gu Lianxing Vokes F M | 1996 | Mineralogical Magazine1996，60，2： | 1 |
| 19 | Pyrite deformation in strati- form lead-zinc deposits of the Canadian Cordillera显示文摘 | GU Lianxing MCCLAY K R 1992 | 1992 | Min-eralium Deposita1992，27，3： | 1 |
| 20 | Hydro- carbon Reservoirs in a Trachyte Porphyry Intrusion in the Eastern Depression of the Liaohe Basin, NE China 显示文摘 | GU Lianxing REN Zuowei WU Changzhi 2002 | 2002 | AAPG Bulletin2002，86，10： | 1 |
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