Geological controls on the natural CO2 accumulation in the Surennuoer Oilfield of the Hailar Basin, China

2021 ◽  
pp. 105319
Author(s):  
Jinxiu Yang ◽  
Ning Qi ◽  
Mark Ireland ◽  
Shuangfang Lu ◽  
Min Wang ◽  
...  
Keyword(s):  
2015 ◽  
Vol 733 ◽  
pp. 140-143
Author(s):  
Jin Hang Cai

Metamorphic rock burial hill reservoir of Beier rift in Hailaer Basin, with large scale reservoir and high output has complex fault system. The fault through going direction roughly is NEE direction, and has wide fault section and lateral quickly changed fault displacement. Metamorphic rock reservoir can be divided into the vertical weathered fracture zone, crack and dissolved pores and caves development belt and tight zone. Accumulation is controlled by hydrocarbon ability of source rock, contacting relationship of source rock and reservoir, oil storage ability of reservoir, and vertical and lateral hydrocarbon migration ability of fault and unconformity surface. And formed top surface weathering crust accumulation pattern which the hydrocarbon migrated laterally along the unconformity surface, and interior reservoir pattern of crack broken zone accumulation which hydrocarbon migrated vertically along fault.


Tectonics ◽  
2019 ◽  
Vol 38 (12) ◽  
pp. 4301-4319 ◽  
Author(s):  
Zheng Ji ◽  
Qi‐An Meng ◽  
Chuan‐Biao Wan ◽  
De‐Feng Zhu ◽  
Wen‐Chun Ge ◽  
...  

2020 ◽  
Vol 51 (5) ◽  
pp. 976-993
Author(s):  
Yuhui Yan ◽  
Baolin Xue ◽  
Yinglan A ◽  
Wenchao Sun ◽  
Hanwen Zhang

Abstract Quantification of runoff change is vital for water resources management, especially in arid or semiarid areas. This study used the Soil and Water Assessment Tool (SWAT) distributed hydrological model to simulate runoff in the upper reaches of the Hailar Basin (NE China) and to analyze quantitatively the impacts of climate change and land-use change on runoff by setting different scenarios. Two periods, i.e., the reference period (before 1988) and the interference period (after 1988), were identified based on long-term runoff datasets. In comparison with the reference period, the contribution rates of both climate change and land-use change to runoff change in the Hailar Basin during the interference period were 83.58% and 16.42%, respectively. The simulation analysis of climate change scenarios with differential precipitation and temperature changes suggested that runoff changes are correlated positively with precipitation change and that the impact of precipitation change on runoff is stronger than that of temperature. Under different economic development scenarios adopted, land use was predicted to have a considerable impact on runoff. The expansion of forests within the basin might induce decreased runoff owing to enhanced evapotranspiration.


2020 ◽  
Vol 55 (3) ◽  
pp. 1750-1762
Author(s):  
Ji‐Chang Zhu ◽  
Qing‐Ren Meng ◽  
You‐Liang Feng ◽  
Hong‐Qi Yuan ◽  
Feng‐Cheng Wu ◽  
...  

2012 ◽  
Vol 86 (1) ◽  
pp. 189-198 ◽  
Author(s):  
LI Junhui ◽  
MENG Qi'an ◽  
LU Shuangfang ◽  
ZHU Defeng ◽  
WU Haibo ◽  
...  
Keyword(s):  

2005 ◽  
Vol 79 (4) ◽  
pp. 459-470 ◽  
Author(s):  
WAN Chuanbiao ◽  
QIAO Xiuyun ◽  
XU Yanbin ◽  
SUN Yuewu ◽  
REN Yanguang ◽  
...  
Keyword(s):  

2018 ◽  
Vol 98 ◽  
pp. 718-732 ◽  
Author(s):  
Han Zheng ◽  
Xiaomeng Sun ◽  
Jiping Wang ◽  
Defeng Zhu ◽  
Xuqing Zhang

2020 ◽  
Author(s):  
Qi-An Meng ◽  
Xue Wang ◽  
Qiu-Li Huo ◽  
Zhong-Liang Dong ◽  
Zhen Li ◽  
...  

Abstract Re–Os radiometric dating of crude oil can be used to constrain the timing of hydrocarbon generation, migration or charge. This approach has been successfully applied to marine petroleum systems; however, this study reports on its application to lacustrine-sourced natural crude oils. Oil samples from multiple wells producing from the Cretaceous Nantun Formation in the Wuerxun-Beier depression of the Hailar Basin in NE China were analysed. Subsets of the Re–Os data are compatible with a Cretaceous hydrocarbon generation event (131.1 ± 8.4 Ma) occurring within 10 Myr of deposition of the Nantun Formation source rocks. In addition, two younger age trends of 54 ± 12 Ma and 1.28 ± 0.69 Ma can be regressed from the Re–Os data, which may reflect the timing of subsequent hydrocarbon generation events. The Re–Os geochronometer, when combined with complementary age dating techniques, can provide direct temporal constraints on the evolution of petroleum system in a terrestrial basin.


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