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| 1 | A hydrocarbon enrichment model and prediction of favorable accumulation areas in complicated superimposed basins in China显示文摘The geologic conditions of superimposed basins in China are very complicated. This is mainly shown by multi-phase structural evolution,multiple sets of source-reservoir-cap rock combinations,multiple stages of hydrocarbon generation and expulsion from source rocks,multi-cycle hydrocarbon enrichment and accumulation,and multi-phase reservoir adjustment and reconstruction. The enrichment,accumulation and distribution of hydrocarbon is mainly controlled by the source rock kitchen,paleoanticline,regional cap rock and intensity of tectonic movement. In this paper,the T-BCMS model has been developed to predict favorable areas of hydrocarbon accumulation in complicated superimposed basins according to time and spatial relationships among five key factors. The five factors include unconformity surface representing tectonic balancing(B) ,regional cap rock representing hydrocarbon protection(C) ,paleo-anticline representing hydrocarbon migration and accumulation(M) ,source rock kitchen representing hydrocarbon generation and expulsion(S) and geological time(T) . There are three necessary conditions to form favorable areas of hydrocarbon accumulation. First,four key factors BCMS should be strictly in the order of BCMS from top to bottom. Second,superimposition of four key factors BCMS in the same area is the most favorable for hydrocarbon accumulation. Third,vertically ordered combination and superimposition in the same area of BCMS should occur at the same geological time. The model has been used to predict the most favorable exploration areas in Ordovician in the Tarim Basin in the main hydrocarbon accumulation periods. The result shows that 95% of the discovered Ordovician hydrocarbon reservoirs are located in the predicted areas,which indicates the feasibility and reliability of the key factor matching T-BCMS model for hydrocarbon accumulation and enrichment. | Pang Xiongqi Meng Qingyang Jiang Zhenxue Liu Luofu Lu Xiuxiang | 2010 | Petroleum Science2010，7，1： | 16 |
| 2 | Trace Fossils from Lower Cambrian Wusongger Formation in Xiaoerbulake Outcrop,Kalpin Area,Xinjiang显示文摘Based on the analysis of trace fossils collected from the typical outcrop of the Lower Cambrian Wusongger Formation in the Kalpin area,ten ichnospecies of six ichnogenus were identified in the upper member of the Wusongger Formation,with most of them being found for the first time.The trace fossils are described seriatim.The ichnospecies are mainly represented by such common trace fossils as Ophiomorpha nodosa,Helminthopsis hieroglyphica,Helminthopsis ichnosp.,Planolites beverleyensis,Planolites vulgaris,Planolites montanus,Palaeophycus striatus,Palaeophycus curvatus?,Cochlichnus anguineus and Rituichnus elongatum.The trace fossils are of high diversity and low abundance,and can be diagnosed as the Cruziana ichnofacies.They can be interpreted as having formed in a shallow water environment. | BAI Zhongkai LU Xiuxiang LIU Xiaoping XIE Qilai LI Jianjiao WU Jianjun | 2012 | Acta Geologica Sinica(English Edition)2012，86，2： | 6 |
| 3 | Hydrocarbon accumulation in deep fluid modified carbonate rock in the Tarim Basin显示文摘The activities of deep fluid are regionalized in the Tarim Basin. By analyzing the REE in core samples and crude oil, carbon isotope of carbon dioxide and inclusion temperature measurement in the west of the Tazhong Uplift in the western Tarim Basin, all the evidence confirms the existence of deep fluid. The deep fluid below the basin floor moved up into the basin through discordogenic fault and volcanicity to cause corrosion and metasomatosis of carbonate rock by exchange of matter and energy. The pore structure and permeability of the carbonate reservoirs were improved, making the carbonate reservoirs an excellent type of deeply buried modification. The fluorite ore belts discovered along the large fault and the volcanic area in the west of the Tazhong Uplift are the outcome of deep fluid action. Such carbonate reservoirs are the main type of reservoirs in the Tazhong 45 oilfield. The carbonate reservoirs in well YM 7 are improved obviously by thermal fluid dolomitization. The origin and territory of deep fluid are associated with the discordogenic fault and volcanicity in the basin. The discordogenic fault and volcanic area may be the pointer of looking for the deep fluid modified reservoirs. The primary characteristics of hydrocarbon accumulation in deep fluid reconstructed carbonate rock are summarized as accumulation near the large fault and volcano passage, late-period hydrocarbon accumulation after volcanic activity, and subtle trap reservoirs controlled by lithology. | LU XiuXiang XIE QiLai YANG Ning LI JianJiao | 2007 | Chinese Science Bulletin2007，52，A01： | 4 |
| 4 | North-south Differentiation of the Hydrocarbon Accumulation Pattern of Carbonate Reservoirs in the Yingmaili Low Uplift,Tarim Basin,Northwest China显示文摘摘要:由分析开发,结构的进化和剩余碳酸盐阶层的水库床的特征,这研究证明剩余在 Yingmaili 焦化阶层低高举在 Tabei 是有利的油和煤气的累积系列(北 Tarim 高举) 高举。有 Yingmaili 的北、南部的斜坡上的烃累积的不同模式低高举。油水库的纵贯的区别被剩余碳酸盐阶层和关键限制的不同岩性学在水库床的发展引起。在 Kuqa 消沉的中生代陆上的有机物和在 Manjiaer 的 Palaeozoic 海洋的有机物北消沉下垂分别地是为北斜坡和南部的斜坡的主要的烃来源岩石。北、南部的斜坡上的烃累积被差别在成熟和这些的热进化历史控制二种有机物。在南部的斜坡上,在早阶段形成的油累积完全被破坏,并且到 Himalayian 的从迟了的 Hercynian 的时期是烃累积的最重要的时间。然而,北斜坡上的烃累积的时间开始了内部埋葬的背斜水库是的 5 妈 B.P 碳酸盐在南部的斜坡上在场,当捱过时,外壳和埋葬 paleo 的山石灰岩地区常见的地形焦化水库在北斜坡上是在场的。北、南部的斜坡分别地有烃累积的不同控制因素。在水库床上的破裂生长是南部的斜坡上的最重要的控制因素;当北斜坡上的烃累积被捱过的外壳和帽子岩石控制时。 | LU Xiuxiang LI Jianjiao ZHAO Fengyun YANG Ning ZHANG Qiucha | 2008 | Acta Geologica Sinica(English Edition)2008，82，3： | 4 |
| 5 | Structural Evolution of the Eastern Qiulitagh Fold and Thrust Belt,Northern Tarim Basin,China显示文摘东方 Qiulitagh 褶层和戳带(EQFTB ) 是活跃 Kuqa 褶层的部分和北 Tarim 盆的戳带。地震思考侧面与地质的表面和练习数据是综合的检验变丑和 EQFTB 的结构风格,特别地第纳干扰器的 deformational 历史 2 煤气的地。地震解释建议 Dongqiu 8 是双结构在被动房顶戳下面开发了的外套,它在中新世的 Jidike 形成从一根尖端线产生了,并且脚底推进从在 Kuqatawu 背斜下面向西延长的一样的 Jidike 形成 evaporite 地区被开始。Dongqiu 5 是在 EQFTB 的西方的部分的弹出式结构,也在 Jidike 形成 evaporite 下面发展了。在 EQFTB 的很轻轻的地下室剧降和陡峭的蘸的地志的斜坡建议 Jidike 形成盐提供有效去耦。在 EQFTB 的强壮的变丑向南显得发展了进一步,在 evaporite 可能正在缺乏的一个区域。自从上新世, EQFTB 在 evaporite 上向南远移动了并且到达了 Yaken 区域。恢复一张平衡剖面图建议越过 EQFTB 的最小的弄短是超过 7800 m。假设这弄短发生在 5.3 妈期间预定平底锅,弄短的率是约 1.47 公里 / 年。 | YANG Minghui JIN Zhijun LU Xiuxiang SUN Dongsheng TANG Xuan PENG Gengxin LEI Ganglin | 2009 | Acta Geologica Sinica(English Edition)2009，83，2： | 2 |
| 6 | Oil and gas accumulations in the Ordovician carbonates in the Tazhong uplift of Tarim Basin, west China显示文摘 | Xiuxiang Lu Zhijun Jin Luofu Liu | 2004 | Journal of Petroleum Science and Engineering2004，41，： | 1 |
| 7 | The tectonics and petroleum system of the Qiulitag fold and thrust belt, northern Tarim basin, NW China显示文摘 | Jin Zhijun Yang Minghui Lu Xiuxiang | 2008 | Marine and Petroleum Geology2008，25，8： | 1 |
| 8 | Oil and gas accumulations in the Ordovician carbonates in the Tazhong Uplift of Tarim Basin,west China 显示文摘 | Lu Xiuxiang Jin Zhijun Liu Luofu | 2004 | Journal of Petroleum Science and Engineering2004，41，1： | 1 |
| 9 | Paleozoic car- bonate hydrocarbon accumulation zones in Tazhong uplift, Tarim basin, western China显示文摘 | Lu Xiuxiang Jiao Weiwei Zhou Xinyuan | 2009 | Energy Exploration & Ex- ploitation2009，27，2： | 1 |
| 10 | Oil and gas accumulations in the Ordovician carbonates in the Tazhong Uplift of Tarim Basin, west China 显示文摘 | Lu Xiuxiang Jin Zhijun Liu Luofu | 2004 | Journal of Petroleum Science and Engineering2004，41，： | 1 |
| 11 | The Silurian play in the Tazhong Uplift, Tarim Basin, northwestern China 显示文摘 | Lu Xiuxiang Fan Qiuhai Zhao Fengyun | 2007 | Marine and Petroleum Geology2007，24，： | 1 |
| 12 | Oil and gas accumulations in the Ordovician carbonates in the Tazhong Uplift of Tarim Basin,west China显示文摘 | Lu Xiuxiang Jin Zhijun Liu Luofu | | 0，，： | 1 |
| 13 | Tectonics and petroleum system of the Qiulitagh fold and thrust belt, northern Tarim basin, NW China 显示文摘 | Jin Zhijun Yang Minghui Lu Xiuxiang | 2008 | Marine and Petroleum Geology2008，25，8： | 1 |
| 14 | The tectonics and pe-troleum system of the Qiulitagh fold and thrust belt,northernTarim basin,NW China显示文摘 | Jin Zijun Yang Minghui Lu Xiuxiang | 2008 | Marine and Petroleum Geology2008，25，： | 1 |
| 15 | Petroleum enrichment characteristics in Ordovician carbonates in Lunnan area of Tarim Basin显示文摘Lunnan heave had experienced denudation during late Caledonian and Hercynian movements and reconstruction during Indosinian movement. Lunnan heave and its circumference areas are located on the direction of petroleum migration, and experienced three reservoir formation cycles that are divided by wave cycle: The first reservoir formation cycle is characterized by breakage, the second by alteration, and the third by enrichment. Three layers of dissolving-cave developed on the vertical in Lunnan area. Development degree of slit-cave system and their connectivity are important factors to control petroleum enrichment in the weathering crust reservoir. The area where dissolving-caves are communicated by silts and faults was a fine petroleum enrichment area, and water was often encountered in the area with isolation cave while drilling because of no oil and gas origin. The top part of the faulted-horst as a leaking area is bearing water area, and the higher part of slope nearing the top part of the | LU Xiuxiang JIN Zhijun ZHOU Xinyuan YANG Ning WANG Qinghua PAN Wenqing | 2004 | Chinese Science Bulletin2004，49，S1： | 0 |
| 16 | Total syntheses of hyperaspidinols A and B enabled by a bioinspired diastereoselective cascade sequence显示文摘A bioinspired acid-triggered hemiacetalization/dehydration/[3 + 3]-type cycloaddition cascade process was disclosed, diastereoselectively furnishing furo[2,3-b]chromene skeleton under mild conditions. The viability of this approach was demonstrated by syntheses of a series of furo[2,3-b]chromene and pyrano[2,3-b]chromene derivatives. The successful total syntheses of two lignan-phloroglucinol hybrids,hyperaspidinols A and B, exemplified the synthetic utility of our biomimetic methodology. | Anquan Zheng Tingting Zhou Sasa Wang Wenge Zhang Xiuxiang Lu Huiyu Chen Haibo Tan | 2022 | Chinese Chemical Letters2022，33，2： | 0 |
| 17 | Summer habitat selection and impacts of human disturbance on leopard cats(Prionailurus bengalensis)显示文摘Introduction:As a consequence of habitat loss and degradation,the leopard cat(Prionailurus bengalensis)in China has become endangered and in need of urgent protection.In situ conservation of leopard cats must be based on an understanding of their habitat selection patterns.We studied the summer habitat of leopard cats using line-transect surveys in the northern Taihang Mountain region surrounding Beijing,China.We compared used plots with non-used plots in elevation,tree canopy,and 20 other ecological variables,and used Vanderploeg��Scavia’s resource selection index(VSI)to analyze habitat preferences.Outcomes/others:Results show that tree canopy,tree height,tree density,and stump quantity of used plots were significantly lower than non-used plots in summer,and that leopard cats preferred habitats located on northern,flat slopes with lower slope,shrub-dominated,dry soil,and less fallen-wood.Leopard cats had a strong tendency to use habitats near human disturbance areas with moderate levels of disturbance intensity.Conclusion:The results suggest that future conservation efforts should emphasize:(1)strengthening the protection and management of forest fringe shrub habitats to improve summer habitat suitability,and(2)environmental education and animal protection campaigns to promote community biodiversity conservation. | Jiayi Wu Jing Wang Yinjiu Zhu Xiangli Bu Rongwei Xiang Qingbin Lu Shaopeng Cui Yinghong Hao Yan Sheng Xiuxiang Meng | 2020 | Ecosystem Health and Sustainability2020，6，1： | 0 |
| 18 | Characteristics and geochemical implications of light hydrocarbons from ultra-deep Ordovician oils in the North Shuntuoguole area, Tarim Basin显示文摘The ultra-deep Ordovician reservoirs in North Shuntuoguole Oilfield(or Shunbei Oilfield)of Sinopec have achieved annual production of one million ton,and the oil&gas in different faults show different physical properties and fluid phases.In this study,the 28 oil samples from the ultra-deep Ordovician were analyzed using whole oil chromatography.The heptane and isoheptane values of the oil samples were in the range of 29.79%‒46.86%and 1.01%-3.06%,respectively,indicating the oils are high mature.The maturity that calculated based on light hydrocarbon values was higher than which calculated by using aromatic hydrocarbon parameters,suggesting the light hydrocarbon maturity mostly reflects the maturity of the late charged hydrocarbon.The 2M-/3M-C5 and 2M-/3M-C_(6) ratios varied in the ranges of 1.41‒1.81 and 0.79-1.09,respectively,and the iC_(5)/nC_(5) and 3M-C_(5)/nC_(6) ratios were 0.31‒0.90 and 0.16-0.37,respectively,indicating that ultra-deep Ordovician reservoirs have not experienced biodegradation.The Mango parameter K_(1) of the oil samples ranges 0.96‒1.01 except for the oil from Well SB4,which suggests that most of the reservoirs have not suffered thermochemical sulfur reduction(TSR).Meanwhile,the oils have not experienced evaporative fractionation since the toluene/nC_(7) and nC_(7)/MCC_(6) ratios range from 0.10-0.38 and 1.50‒1.80,respectively.The close correlation between P_(3) and P_(2)+N_(2) and between P_(2) and N_(2)/P_(3) indicates that the oils from different faults have the same origin.According to the characteristics of LHs rich in n-alkane,as well as other biomarkers,such as aryl isoprenoids,and aromatic hydrocarbon parameters,the oil originated from the source rock of Lower Cambrian Yu’ertusi Formation.Meanwhile,the source rocks in different fault zones slightly differed in organic facies. | Li DONG Anlai MA Huixi LIN Lu YUN Weilong PENG Xiuxiang ZHU | 2022 | Frontiers of Earth Science2022，16，3： | 0 |
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