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| 1 | Relationship between the later strong gas-charging and the improvement of the reservoir capacity in deep Ordovician carbonate reservoir in Tazhong area, Tarim Basin显示文摘Some large-scale oil-gas fields have recently been discovered in marine carbonate in China, especially the significant discoveries in deep reservoir that reveals a favorable exploration prospect. Tazhong area is the first-order tectonic unit in Tarim Basin, where there are nearly trillion cubic meters of natural gas resources in the Ordovician limestone reef flat complex in Lianglitage Formation. The reservoir is shelf edge reef flat complex, characterized by ultra-low porosity, low permeability and strong heterogeneous, with a current burial depth of 4500―6500 m. Studies find that the formation and distribution of deep reservoir of the Lianglitage Formation were controlled not only by the early high-energy sedimentary facies and corrosion, but the fracture network formed by the strong gas-charging process since the Himalayan epoch, which played an important role in optimizing and improving reservoir properties. This paper discusses the relationship between the strong later gas-charging and the improvement of the reservoir capacity in deep Ordovician carbonate reservoir, and also builts the corresponding mechanisms and modes, which is favorable for the prediction and evaluation of the advantageous exploration targets. | ZHAO WenZhi ZHU GuangYou ZHANG ShuiChang ZHAO XueFeng SUN YuShan WANG HongJun YANG HaiJun HAN JianFa | 2009 | Chinese Science Bulletin2009，54，17： | 31 |
| 2 | Depositional architecture of the late Ordovician drowned carbonate platform margin and its responses to sea-level fluctuation in the northern slope of the Tazhong region, Tarim Basin显示文摘The Tazhong Uplift of the late Ordovician is a drowned rimmed carbonate platform. The carbonate rock of the late Ordovician Lianglitage Formation in the northern slope of the Tazhong region is one of the significant petroliferous intervals. Based on petrofacies, depositional cycles, natural gammaray spectrometry and carbon/oxygen isotope data from the Lianglitage Formation, one 2nd-order, three 3rd-order and several 4th-order sequences have been recognized, and the late Ordovician relative sealevel fluctuation curve has been established. The sequences O 3 l-1 and O 3 l-2 on the platform are composed of highstand and transgressive systems tracts, but lack the lowstand systems tract. The sequence O 3 l-3 is a drowning sequence. The sequence O 3 l-1 overlapped the eroded slope and pinched out to the northwest and landward. The highstand systems tract in the sequence O 3 l-2 consists of low-angle sigmoid and high-angle shingled progradation configuration. Major sedimentary facies of the Lianglitage Formation include reef and shoal in the platform margin and lagoon, which can be subdivided into coral-sponge-stromatoporoid reef complex, sand shoal, lime mud mound, and intershoal sea. Reefs, sand shoals and their complex are potential reservoir facies. The reefs and sand shoals in the sequence O 3 l-1 developed in the upper of its highstand systems tract. In the sequence O 3 l-2, the highstand systems tract with an internal prograding configuration is a response to the lateral shifting of the complex of reef and sand shoal. The transgressive systems tract, in particular the sand shoals, developed widely on the slope of the platform margin and interior. The reefs in the sequence O 3 l-3 migrated towards high positions and formed retrograding reefs in the western platform and low relief in the platform interior. Basinward lateral migration of the reefs and pure carbonate rock both characterize highstand systems tract and show that the rise of the relative sea-level was very slow. Shingled prograding stacking pattern of the 4th-order sequences and reefs grow horizontally, which represents the late stage of highstand systems tract and implies relative sealevel stillstand. Reefs migrating towards high land and impure carbonate rock both indicate transgressive systems tract and suggest that the relative sea-level rose fast. Erosional truncation and epidiagenetic karstification represent a falling relative sea-level. The relative sea-level fluctuation and antecedent palaeotopography control the development and distribution of reef complexes and unconformity karst zones. Currently, the composite zone of epidiagenetic karstic intervals and high-energy complexes of reefs and sand shoals with prograding configuration is an important oil and gas reservoir in the northern slope of the Tazhong carbonate platform. | Yang Xiaofa Lin Changsong Yang Haijun Han Jianfa Liu Jingyan Zhang Yanmei Peng Li Jing Bing Tong Jianyu Wang Haiping Li Huanpu | 2010 | Petroleum Science2010，7，3： | 8 |
| 3 | Differences of Hydrocarbon Enrichment between the Upper and the Lower Structural Layers in the Tazhong Paleouplift显示文摘Tazhong paleouplift 被划分成上面并且更低的结构的层,在奥陶纪碳酸盐岩石的顶由不顺从表面跳了。在从不同部分的二层的水库在数字变化,类型和储备,而是机制以前很少被研究。因此,机制的解释将在 Tazhong paleouplift 支持石油探索。在学习进化和 Tazhong paleouplift 的水库分发以后,在晚古苏格兰的、迟了的 Hercynian 和喜玛拉雅的时期的进化导致了,这被结束上面并且更低的结构的层。这也被定义在上面的结构的层,结构并且, stratigraphic 重叠水库为更低的结构的层在顶和 paleouplift 的上面的部分被开发,它被油水库统治, lithological 水库在 paleouplift 的更低的部分被开发,它被煤气的水库,和更多统治储备在更低的结构的层被发现比上面。通过累积条件的比较分析上面并且更低的结构的层,丰富差别的机制清楚地被解释。更低的结构的层的水库和封口条件比上面的层的那些好,它是更多的水库在前者被发现了的原因。在搬运人系统类型,陷井类型和收费时期在之间的差别上面并且更低的结构的层在水库类型和分布导致差别。一个累积模型为 Tazhong paleouplift 被建立。为上面的结构的层,,结构的水库和 stratigraphic 重叠水库为更低的结构的层在 paleouplift 的上面的部分被形成,捱过的外壳水库在顶被形成,礁石公寓水库在侧面的边缘上被形成,石灰岩地区常见的地形和里面水库在 paleouplift 的更低的部分被形成。 | JIANG Zhenxue YANG Haijun LI Zhuo PANG Xiongqi HAN Jianfa LI Dongxu HUANG Yuyan | 2010 | Acta Geologica Sinica(English Edition)2010，84，5： | 7 |
| 4 | Seismic attributes and integrated prediction of fractured and caved carbonate reservoirs in the Tarim Basin,China显示文摘The carbonate reservoirs in the Tarim Basin are characterized by anisotropy and strong heterogeneity.Combined with an integrated analysis of data from seismic,geology,and drilling results,a series of attributes which are suitable for fractured and caved carbonate reservoir prediction is discussed,including amplitude,coherence analysis,spectra decomposition,seismic absorption attenuation analysis and impedance inversion.Moreover,3-D optimization of these attributes is achieved by integration of multivariate discriminant analysis and principle component analysis,where the logging data are taken as training samples.Using the optimized results,the spatial distribution and configuration features of the caved reservoirs can be characterized in detail.This technique not only improves the understanding of the spatial distribution of current reservoirs but also provides a significant basis for the discovery and production of carbonate reservoirs in the Tarim Basin. | Liu Lifeng Sam Zandong Sun Yang Haijun Han Jianfa Gao Hongliang Jing Bing Zhu Xinghui | 2011 | Petroleum Science2011，8，4： | 6 |
| 5 | Accumulation process and model for the Ordovician buried hill reservoir in the western Lunnan area,the Tarim Basin显示文摘The Ordovician buried hill reservoir in the western Lunnan area, a type of dissolved fracture and cavernous reservoir, is mainly composed of heavy oil. The oil is the mixture sourcing from the Middle-Lower Cambrian and Middle-Lower Ordovician, with three stages of pool forming process: (1) the destruction and parallel migration/accumulation during the late Caledonian to early Hercynian; (2) the oil and gas accumulation during the late Hercynian characterized by adjustment upward along faults and parallel migration/accumulation; (3) the formation of heavy oil during the latest Hercynian. The Ordovician buried hill reservoir is affected by the diffusion of light oil and gas but had no hydrocarbon charging during the late Yanshan period to Himalayan period, but in this period, formed the association of heavy oil and dissolved gas cracked from crude oil with dry coefficient of 0.91-0.96. The study on accumulation process of the Ordovician buried hill reservoir has important implications for the exploration potential of early oil and gas accumulation in the cratonic area of the Tarim Basin. | ZHAO MengJun PAN WenQing HAN JianFa LIU ShaoBo QIN ShengFei ZHANG BaoMin | 2007 | Chinese Science Bulletin2007，52，A01： | 6 |
| 6 | The application of amplitude-preserved processing and migration for carbonate reservoir prediction in the Tarim Basin,China显示文摘Conventional seismic exploration method based on post-stack data usually fails to identify the distribution of fractured and caved carbonate reservoirs in the Tarim Basin,so the rich pre-stack information should be applied to the prediction of carbonate reservoirs.Amplitude-preserved seismic data processing is the foundation.In this paper,according to the feature of desert seismic data (including weak reflection,fast attenuation of high frequency components,strong coherent noises,low S/N and resolution),a set of amplitude-preserved processing techniques is applied and a reasonable processing flow is formed to obtain the high quality data.After implementing a set of pre-stack amplitude-preserved processing,we test and define the kernel parameters of amplitude-preserved Kirchhoff PSTM (pre-stack time migration) and subsequent gathers processing,in order to obtain the amplitude-preserved gathers used to the isotropic pre-stack inversion for the identification of caved reservoirs.The AVO characteristics of obtained gathers fit well with the synthetic gathers from logging data,and it proves that the processing above is amplitudepreserved.The azimuthal processing techniques,including azimuth division and binning enlargement,are implemented for amplitude-preserved azimuthal gathers with the uniform fold.They can be used in the anisotropic inversion to detect effective fractures.The processing techniques and flows are applied to the field seismic data,and are proved available for providing the amplitude-preserved gathers for carbonate reservoir prediction in the Tarim Basin. | Sam Zandong Sun Yang Haijun Zhang Yuanyin Han Jianfa WangDan Sun Wenbo Jiang Shan | 2011 | Petroleum Science2011，8，4： | 6 |
| 7 | Large-scale Tazhong Ordovician Reef-flat Oil-Gas Field in the Tarim Basin of China显示文摘Tazhong 礁石公寓油气体地是在中国发现的第一块大规模奥陶纪器官的礁石类型油气体地。它的器官的礁石在早迟了的奥陶纪 Lianglitag 形成被开发,并且是在中国发现的 coral-stromatoporoid hermatypic 社区的第一大礁石。器官的礁石和站台边缘谷物银行组成礁石公寓建筑群,主要由 biolithites 和谷物石头组成。biolithites 能被分类进 framest 那, bafflest,绑石头等等。建筑群的主要身体从 Tazhong-24 躺在井附近到 Tazhong-82, trending 西北与从 100 ~ 300 m 的厚度,长度大约 220 km 和宽度 5 10 km。它是一座礁石公寓石版印刷逻辑烃水库,与很复杂的烃分布:与本地油水库总体上是一座煤气的冷凝物水库。烃分发被礁石建筑群控制,通常定位了在上面建筑群的 100 200 m 部分,并且主要在沿着建筑群的 banded 形状。在侧面上,水库显示出一个成层的特征,与到西北的从东南的几乎 2200 m 的高度差别。石油累积被石灰岩地区常见的地形水库床和东北罢工滑倒差错带控制。全部的地质的储备在 2007 到达了 297.667 山。 | ZHOU Xinyuan WANG Zhaoming YANG Haijun ZHANG Lijuan HAN Jianfa WANG Zhenyu | 2009 | Acta Geologica Sinica(English Edition)2009，83，1： | 3 |
| 8 | Accumulation characteristics and the main controlling factors of Lunnan multilayer oil province,Tarim Basin,China显示文摘Lunnan region is a large-scale paleohigh with many coexisting oil and gas bearing series.At present, about 2 billions tons of proved,probable and possible oil and gas reverses have been proved there.Eight oil and gas bearing series have been found in the Ordovician,Carboniferous,Triassic and Jurassic of Lunnan region,they all bear the characteristics of large-scale multilayer oil-gas province.Ordovician is the main reservoir series where over 0.8 billion tons of oil geologic reserves were discovered,and a super large-scale marine carbonate oil and gas field has formed.Reservoir space of the carbonate reservoirs is mainly composed of dissolved hole,dissolved pore and fracture in Lunnan paleo-burial hill.Generally, dissolved holes are widely distributed among them.Reservoir developments are mainly controlled by karstification and tectonic disruption.Due to the similar geochemical characters,the Ordovician,Carboniferous,Triassic and Jurassic oil and gas reservoirs present the same oil source rock of Mid-Upper Ordovician,the latter except Ordovician are mostly of secondary oil and gas reservoirs migrated vertically by faults during the process of multiple phase tectonic movement,adjustment and reconstruction. Lunnan composite oil and gas accumulation region is situated in the vicinity of large-scale hydrocarbon generation depressions in three directions,ample oil and gas from hydrocarbon generation depressions supplied the adjacent oil and gas reservoirs once.Hereby,the succeed paleohigh is the long-term hydrocarbon accumulation region,which is favor for the formations of high quality reservoirs,fault systems and huge-scale composite oil and gas accumulation. | YANG HaiJun1 ,2&HAN JianFa 1,2 1Resources School of China University of Geosciences,Wuhan 430074,China 2Research Institutes of Tarim Oilfield Company,PetroChina,Korla 841000,China | 2008 | Science China Earth Sciences2008，51，S1： | 3 |
| 9 | Ordovician Carbonate Reservoir Bed Characteristics and Reservoir-Forming Conditions in the Lungudong Region of the Tarim Basin显示文摘在 Tarim 盆的东北部分的 Lungudong 区域的奥陶纪碳酸盐水库床的基本特征详细被描述,油和气体的形成水库的条件被收集并且整理大量数据 preliminarily 在这份报纸讨论。碳酸盐水库床主要被开发在开站台并且站台边缘的外形;水库床有大变化在并且物理性质的低平均价值;主要类型第二是有破裂多孔的类型的折断的水库床。水库床发展被沉积外形,构造活动和 karstification 的分发主要控制。而在这个区域的烃的累积和分发被一个有益的结构的地点,好 reservoir-caprock 联合和一个有利搬运系统控制,与地区水平地描绘的分发和带垂直地,油和气体主要在区域被集中与结构高举,浓密地发达的破裂,并且表面石灰岩地区常见的地形,一个垂直 vadose 地区,和水平潜流 palaeokarst 系上带子。 | GU Qiaoyuan PANG Xiongqi LIU Luofu YANG Haijun WANG Ying JIANG Zhenxue XIANG Caifu HAN Jianfa | 2010 | Acta Geologica Sinica(English Edition)2010，84，5： | 2 |
| 10 | Hydrocarbon charging of the Ordovician reservoirs in Tahe-Lunnan area, China显示文摘The Tahe-Lunnan hydrocarbon province is China's largest region with oil-and-gas-producing marine carbonate rocks. However, in terms of multi-source hydrocarbon generation, multi-episode reservoir adjustment and reconstruction, it remains unsettled how to determine the geological period of primary hydrocarbon filling of the Ordovician reservoir in this region. Based on the analysis of distribution and properties of reservoir, hydrocarbon filling of the Cambrian source rocks in the Late Caledon stage has largely been destroyed. However, hydrocarbon filling of the Middle Ordovician source rocks in the Early Carboniferous resulted in the major body of crude oil. During the charging process, the hydrocarbons were oxidatively degraded to heavy oil due to the poor closure conditions, which is corroborated by homogenization temperature of inclusions. Moreover, the capturing of hydrocarbon inclusions with high-temperature does not represent the filling of mature petroleum in the later period, but represents the result of the natural gas containing light fraction. Therefore, the Tahe-Lunnan area underwent two hydrocarbon filling processes, and the invasion of excessive dry gas led to a gas-washing fractionation upon the original Ordovician reservoirs. | WU Nan CAI ZhongXian YANG HaiJun WANG ZhenQi LIU XianFeng HAN JianFa | 2013 | Science China Earth Sciences2013，56，5： | 1 |
| 11 | Tracing hydro carbons migration pathway in carbonate rock in Lunnan-Tahe oilfield显示文摘 | Zhou Xinyuan Jiao Weiwei Han Jianfa | 2010 | Energy Exploration & Exploitation2010，28，4： | 1 |
| 12 | Biodegradation of 2,4,6-trinitrophenol (picric acid) in a biological aerated filter (BAF)显示文摘 | Shen Jinyou He Rui Yu Hongxia Wang Lianjun Zhang Jianfa Sun Xiuyun Li Jiansheng Han Weiqing Xu Lu | 2009 | Bioresource Technology2009，，100： | 1 |
| 13 | Trac-ing hydrocarbons migration pathway in carbonate rock inLunnan-Tahe Oilfield显示文摘 | Zhou Xinyuan Jiao Weiwei Han Jianfa | 2010 | Energy Exploration & Develop-ment2010，28，4： | 1 |
| 14 | Characteristics of Paleozoic clastic reservoirs and the relationship with hydrocarbon accumulation in the Tazhong area of the Tarim Basin, west China显示文摘In order to predict favorable exploration areas of the Paleozoic, Carboniferous and Silurian clastic reservoirs in the Tazhong area of the Tarim Basin, west China, we studied the basic characteristics of Paleozoic clastic reservoirs in the Tazhong area based on a lot of data. Several issues about the hydrocarbon accumulation related to the reservoirs were also discussed. The results were concluded that: the high-value areas of the porosity and permeability of clastic reservoirs were located in the southeast of the Tazhong area; the content of cement (carbonate cement in particular) was the main factor controlling the porosity and permeability of clastic reservoirs; the hydrocarbon distributions of Carboniferous and Silurian clastic reservoirs were closely related to the porosity and permeability; the favorable hydrocarbon accumulation areas of the two sets of strata were located in the southeast of this area, especially in the updip pinch-out area. | Wang Zhaoming Liu Luofu Yang Haijun Wang Weili ZhangBaoshou Han Jianfa | 2010 | Petroleum Science2010，7，2： | 1 |
| 15 | Control of hydrocarbon accumulation by Lower Paleozoic cap rocks in the Tazhong Low Rise, Central Uplift, Tarim Basin, West China显示文摘Despite the absence of regional cap rocks in the Lower Paleozoic for the entire Tazhong Low Rise, several sets of effective local cap rocks are well preserved on the Northern Slope. Of these the best is the Ordovician mudstone of the Sangtamu Formation; the second is the Silurian Red Mudstone Member of the Tatairtag Formation and the marl of the Ordovician Lianglitag Formation; and the third is the gray mudstone of the Silurian Kepingtag Formation. The dense limestone of the Ordovician Yingshan Formation and the gypsum of the Middle Cambrian have shown initial sealing capacity. These effective cap rocks are closely related to the distribution of Lower Palaeozoic hydrocarbons in the Tazhong Low Rise. With well-preserved Sangtamu Formation mudstone and its location close to migration pathways, rich Lower Paleozoic hydrocarbon accumulation can be found on the Northern Slope. Vertically, most of the reserves are distributed below the Sangtamu Formation mudstone; areally, hydrocarbons are mainly found in the areas with well-developed Sangtamu Formation mudstone and Lianglitag Formation marl. Burial history and hydrocarbon charging history show that the evolution of Lower Palaeozoic cap rocks controlled the accumulation of hydrocarbon in the Tazhong Low Rise. Take the Red Mudstone Member of the Tatairtag Formation and Sangtamu Formation mudstone for examples: 1) In the hydrocarbon charging time of the Late Caledonian-Early Hercynian, with top surfaces at burial depths of over 1,100 m, the cap rocks were able to seal oil and gas; 2) During the intense uplifting of the Devonian, the cap rocks with top surfaces at burial depths of 200-800 m and 500-1,100 m respectively were denuded in local areas, thus hydrocarbons trapped in earlier time were degraded to widespread bitumen; 3) In the hydrocarbon charging time of the Late Hercynian and Himalayan, the top surfaces of the cap rocks were at burial depths of over 2,000 m without intense uplifting and denudation thereafter, so trapped hydrocarbons were preserved. Based on cap rocks, the Ordovician Penglaiba Formation and Lower Cambrian dolomite could be potential targets for exploration on the Tazhong Northern Slope, and combined with hydrocarbon migration, less risk would be involved. | Zhang Yanping Lü Xiuxiang Yang Haijun Han Jianfa Lan Xiaodong Zhao Yue Zhang Jinhui | 2014 | Petroleum Science2014，11，1： | 1 |
| 16 | Origin and growth mechanisms of strike-slip faults in the central Tarim cratonic basin, NW China显示文摘Through fault structure analysis and chronology study, we discuss the origin and growth mechanisms of strike-slip faults in the Tarim Basin.(1) Multiple stages strike-slip faults with inherited growth were developed in the central Tarim cratonic basin. The faults initiation time is constrained at the end of Middle Ordovician of about 460 Ma according to U-Pb dating of the fault cements and seismic interpretation.(2) The formation of the strike-slip faults was controlled by the near N-S direction stress field caused by far-field compression of the closing of the Proto-Tethys Ocean.(3) The faults localization and characteristics were influenced by the pre-existing structures of the NE trending weakening zones in the basement and lithofacies change from south to north.(4) Following the fault initiation under the Andersonian mechanism, the strike-slip fault growth was dominantly fault linkage, associated with fault tip propagation and interaction of non-Andersonian mechanisms.(5) Sequential slip accommodated deformation in the conjugate strike-slip fault interaction zones, strong localization of the main displacement and deformation occurred in the overlap zones in the northern Tarim, while the fault tips, particularly of narrow-deep grabens, and strike-slip segments in thrust zones accumulated more deformation and strain in the Central uplift. In conclusion, non-Andersonian mechanisms, dominantly fault linkage and interaction, resulted in the small displacement but long intraplate strike-slip fault development in the central Tarim Basin. The regional and localized field stress, and pre-existing structures and lithofacies difference had strong impacts on the diversity of the strike-slip faults in the Tarim cratonic basin. | WU Guanghui MA Bingshan HAN Jianfa GUAN Baozhu CHEN Xin YANG Peng XIE Zhou | 2021 | Petroleum Exploration and Development2021，48，3： | 0 |
| 17 | Porous framework materials for energy&environment relevant applications:A systematic review显示文摘Carbon peaking and carbon neutralization trigger a technical revolution in energy&environment related fields.Development of new technologies for green energy production and storage,industrial energy saving and efficiency reinforcement,carbon capture,and pollutant gas treatment is in highly imperious demand.The emerging porous framework materials such as metal–organic frameworks(MOFs),covalent organic frameworks(COFs)and hydrogen-bonded organic frameworks(HOFs),owing to the permanent porosity,tremendous specific surface area,designable structure and customizable functionality,have shown great potential in major energy-consuming industrial processes,including sustainable energy gas catalytic conversion,energy-efficient industrial gas separation and storage.Herein,this manuscript presents a systematic review of porous framework materials for global and comprehensive energy&environment related applications,from a macroscopic and application perspective. | Yutao Liu Liyu Chen Lifeng Yang Tianhao Lan Hui Wang Chenghong Hu Xue Han Qixing Liu Jianfa Chen Zeming Feng Xili Cui Qianrong Fang Hailong Wang Libo Li Yingwei Li Huabin Xing Sihai Yang Dan Zhao Jinping Li | 2024 | Green Energy & Environment2024，9，2： | 0 |
| 18 | Introduction to the special section:Recent advancement on integrated carbonate reservoirs prediction with complex secondary storage space显示文摘Carbonate reservoirs in Western China show tremendous exploration and development potential.These have become the key area for oil and gas reserves addition and sustainable resource development for China.Compared to conventional carbonate reservoirs,prediction of this kind of reservoir predominated by secondary storage is much more difficultand presents significant challenges. | Yuanyin Zhang Sam Zandong Sun Haijun Yang Haiyang Wang Jianfa Han et al. | 2011 | Petroleum Science2011，8，4： | 0 |
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