Haisheng Yi

First Hospital of Jilin University

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Guoqing Xia

Jiangsu University

Chihua Wu

Chengdu University of Technology

Gaojie Li

Mianyang Normal University

Chengshan Wang

China University of Geosciences (Beijing)

Yi Fan

Xiamen University

Michael Wagreich

University of Vienna

Changjun Ji

Shanghai Mental Health Center

Xuejuan Da

Chongqing University of Science and Technology

Guiwen Xu

Chinese Academy of Sciences

Xixi Zhao

Sichuan Normal University

Cooperative Institutions

Chengdu University of Technology

Chinese Academy of Sciences

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation

Jilin University

Chinese Academy of Geological Sciences

China Geological Survey

University of Chinese Academy of Sciences

First Hospital of Jilin University

Nanjing University

Ministry of Natural Resources

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A dataset of gas reservoir microscopic images in Xujiahe Formation in northeast Sichuan Basin

China Scientific Data (2023)

Xinlan DU Haisheng Yi

The gas reservoir in Xujiahe Formation in northeast Sichuan Basin holds promising potential for exploration and development. In this paper, we collected and sorted the microscopic image data of the clastic reservoir of Xujiahe Formation gas reservoir in the study area, so as to further study the petrological characteristics, diagenesis, reservoir space and physical properties of the region. The reservoir rocks are mainly lithic sandstone, lithic arkose sandstone and quartz sandstone. There are intergranular solution pores, residual intergranular solution pores, intragranular solution pores, clay mineral intergranular (solution) pores and various microfractures in the reservoir space. According to the observation of the cast thin section, the pores are relatively undeveloped, while some thin sections (micro-cracks) are relatively developed. Based on thin section identification and observation, the sandstone reservoirs of Xujiahe Formation in the study area have undergone processes such as compaction, cementation, dissolution and tectonic fracture. This dataset can provide a direct source for the comparative analysis and reference of sandstone image data. Moreover, it can serve as a benchmark for the intelligent identification of lithology.

Thin section

Lithology

Stratum

Cementation (geology)

Lithic fragment

10.11922/11-6035.csd.2021.0088.zh

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Cenozoic Exhumation History of the East Kunlun Orogenic Belt Constrained by Apatite Fission‐Track Thermochronology

Acta Geologica Sinica - English Edition (2018)

Wei Yang Guoqing Xia Chihua Wu Haisheng Yi

Thermochronology

Fission track dating

10.1111/1755-6724.13606

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Sedimentary Record of the Planation Surface in the Hoh Xil Region of the Northern Tibet Plateau

Acta Geologica Sinica - English Edition (2000)

Haisheng Yi Chengshan Wang Zhiwu Li Liu Zhifei Wang Shifeng

Abstract Miocene marl is the most widespread Tertiary stratigraphic record in the northern Tibet Plateau, termed the Wudaoliang Group in the Hoh Xil region and the correlative Suonahu Formation in the Qiangtang region. The uniform marl overlies red beds of the Eocene‐Oligocene Fenghuoshan Group. The Wudaoliang Group is generally 100–400 m thick, but the thickest strata are 700–1300 m, located in the Haidinghu (Haiding Lake) and Tuotuohe (Tuotuo River) regions respectively. Based on observations from eight measured sections and outcrops, the thin‐bedded marl, which varies in colour from grey‐white to light brown‐grey, is explained as a large‐scale or serial lacustrine deposit stretching throughout northern Tibet. The Wudaoliang Group commonly crops out on geographic lowland at an average elevation of 4600 m above sea level within the mountain chains, showing concordant summit levels, e.g. the Fenghuoshan and Bairizhajia Mountains. These mountains with a flat ridge are considered to be remains of the palaeo‐planation surface. However, the spatial distribution of the Wudaoliang Group is not confined by the current mountain‐basin landform configuration. We have observed the Miocene Wudaoliang Group marl exposed on a 5233 m‐high mountain peak. The largest difference in height between the current lake level and the mesa crest is 600 m; the maximum dip angle is 25°, but usually below 10°, which is obviously different from the Fenghuoshan Group red beds with moderate to strong structural deformation. The horizon of the Wudaoliang Group thin‐bedded marl and its widespread occurrence throughout the northern Tibetan Plateau can only be reasonably inferred to a sedimentary record relevant to the palaeo‐planation. Its deposition occurred on primary land floor by erosion at 20 Ma and its bed surface is a typical sign of geomorphic rise and collapse after the erosion.

Marl

Outcrop

Landform

10.1111/j.1755-6724.2000.tb00498.x

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Citations (13)

Biomarkers of Middle to Late Jurassic marine sediments from a canonical section: New records from the Yanshiping area, northern Tibet

Marine and Petroleum Geology (2014)

Lan Chen Guiwen Xu Xuejuan Da Changjun Ji Haisheng Yi

Sterane

Dinoflagellate

Dominance (genetics)

Terrigenous sediment

10.1016/j.marpetgeo.2013.12.018

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Citations (11)

Organic geochemistry characteristics of Jurassic black shales from the Amdo area, northern Tibet, China

Acta Geochimica (2022)

Guiwen Xu Lan Chen Weiguang Zhu Xuejuan Da Zhangxiong Zhu

Marl

Sterane

10.1007/s11631-022-00537-y

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Mineral phase changes and depositional model of sedimentary manganese deposits in Dounan area of southeastern Yunnan

Zhongguo dizhi (2011)

Haisheng Yi

The Dounan manganese deposit is a large-size sedimentary manganese deposit in southeastern Yunnan,and a study of its genesis can reveal the model of sedimentary manganese deposits in southeastern Yunnan.Samples from the Dounan manganese deposit were systematically studied by means of manganese phase analysis and IR spectroscopy.Based on a study of the relationship between the type of manganese and redox interface,the authors hold that the model of sedimentary manganese deposits is controlled by redox interface changes caused by sea level changes.

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Citations (2)

Recognition, genesis and evolution of manganese ore deposits in southeastern China

Ore Geology Reviews (2013)

Qiuding Du Haisheng Yi Bo Hui LI Sheng-jun Guoqing Xia

Ladinian

Cathodoluminescence

10.1016/j.oregeorev.2013.05.001

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Citations (10)

Tectonic and sedimentary evolution of basins in the northeast of Qinghai-Tibet Plateau and their implication for the northward growth of the Plateau

Palaeogeography Palaeoclimatology Palaeoecology (2006)

Lidong Zhu Chengshan Wang Hongbo Zheng Xiang Fang Haisheng Yi

Tectonic subsidence

10.1016/j.palaeo.2006.06.019

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Citations (108)

Magnetostratigraphic Studies of Tertiary Continental Redbeds in Wulanwula Lake Area of Northern Tibetan Plateau and Their Geologic Significance

Acta Geosicientia Sinica (2004)

Haisheng Yi

A total of 156 individual oriented samples were collected from Tertiary continental red beds in the upper lithologic unit of the Fenghuoshan Group within Wulanwula Lake area, northern Tibetan plateau. Rock magnetic measurement and demagnetization analysis were performed at the paleomagnetism laboratories of the University of California, Santa Cruz, USA. Most samples exhibited two components of magnetization in thermal demagnetization experiments. The most stable high-unblocking temperature components were isolated and passed positive reversal and fold tests at the 95% confidence level. The polarity patterns from the red bed sequence show that a reliable magnetostratigraphy can be established. Its normal polarity intervals are correlated with C23n-C20n of the geomagnetic polarity time scale (GPTS). The age of measured Fenghuoshan Group section is paleomagnetically dated as 52～42 Ma (Middle Eocene) and defined by K-Ar isotopic dating of discrete intrusion dikes. This suggests that the Fenghuoshan Group is a diachronic lithostratigraphic unit across paleo-suture zone and its deposition occurred synchronously with the Indian and Eurasian continental collision.

Magnetostratigraphy

Red beds

Lithology

Polarity (international relations)

Dike

Paleogene

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Citations (7)

Analysis on Application of Casual Connections between Database Tables

Journal of Wuhan Polytechnic (2012)

Haisheng Yi

The paper holds that relational database sets up connection between tables in the database.And once the tables are connected,they can work coordinately to solve practical problems.In database operation,multiple tables can accomplish assigned tasks coordinately.The paper specifies how it can be used in daily work.

Casual

Table (database)

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