The Lenghu tectonic belt is located at or near the northern margin in the Qaidam Basin,which is an intracontinental composite basin evolved during the Mesozoic and Cenozoic epochs.The Lower Jurassic is considered a go...The Lenghu tectonic belt is located at or near the northern margin in the Qaidam Basin,which is an intracontinental composite basin evolved during the Mesozoic and Cenozoic epochs.The Lower Jurassic is considered a good source rock with a wide distribution.Since the deposit of the Lower Jurassic hydrocarbon source rock,the basin has undergone many tectonic events of subsidence and uplift.The source rocks in the Lengke-1 well,have experienced a complicated tectonic-burial history during which different hydrocarbon generation(HG) evolutions have taken place.We have investigated the history of burying,heating and hydrocarbon generation of the Lower Jurassic source rocks,not just on the basis of tectonic disturbance and deep burial,but also from new studies in fluid inclusion measurements and the application of numerical simulation with EASY%Ro.Our study reveals the evolution process,tectonic episodes and the strength of the HG of the Jurassic source rock.We conclude that twice HG processes have taken place since the Lower Jurassic formation and infer from that the important conclusion that more HG of the Lower Jurassic source rock took place during the Eocene-Miocene epochs.Finally,we discuss the oil and gas tarp formation and destruction in the Lenghu tectonic belt and point out that more attention should be paid to the thrust faults,which formed during the late Himalayan epoch.展开更多
The Lenghu area is one of the most crucial tectonic belts for oil and gas exploration in the Qaidam Basin.However,reservoir distribution and the factors controlling petroleum accumulation in this area have not been st...The Lenghu area is one of the most crucial tectonic belts for oil and gas exploration in the Qaidam Basin.However,reservoir distribution and the factors controlling petroleum accumulation in this area have not been studied in detail.In this paper,the structural characteristics and controlling factors of oil and gas accumulation in the Lenghu belt are investigated based on seismic profiles combined with drilling logs and microphotographs data.Results indicate that the Lenghu belt has thick source rocks and has preserved hydrocarbon generation conditions.Moreover,structural characteristics and lithology are the key factors controlling the reservoir distribution.The production of oil and gas layers are mainly distributed in high structural points and weak stress zones.The fracture zones and the weak stress zones are the potential places for the distribution of oil and gas reservoirs.展开更多
冷湖地区因干旱少雨、晴天数多、云量覆盖少等特点,引起了天文学家的高度关注。2018年开始在冷湖赛什腾山开展光学视宁度测量,几年测量结果表明赛什腾山光学台址特性可比肩世界著名光学台址。为进一步了解赛什腾天文台址的电磁环境特性...冷湖地区因干旱少雨、晴天数多、云量覆盖少等特点,引起了天文学家的高度关注。2018年开始在冷湖赛什腾山开展光学视宁度测量,几年测量结果表明赛什腾山光学台址特性可比肩世界著名光学台址。为进一步了解赛什腾天文台址的电磁环境特性,开展了无人值守无线电干扰RFI(Radio Frequency Interference)测量设备的研制以及在赛什腾山天文台址的电磁环境监测。文章主要介绍基于研制的0.1~18 GHz频段RFI测量系统,在冷湖赛什腾山天文台址规划D点(海拔4055 m)开展为期超过一年的RFI测量,以及测量结果的评估。展开更多
基金supported by the Natural Oil & Gas Stratagem Tap of China
文摘The Lenghu tectonic belt is located at or near the northern margin in the Qaidam Basin,which is an intracontinental composite basin evolved during the Mesozoic and Cenozoic epochs.The Lower Jurassic is considered a good source rock with a wide distribution.Since the deposit of the Lower Jurassic hydrocarbon source rock,the basin has undergone many tectonic events of subsidence and uplift.The source rocks in the Lengke-1 well,have experienced a complicated tectonic-burial history during which different hydrocarbon generation(HG) evolutions have taken place.We have investigated the history of burying,heating and hydrocarbon generation of the Lower Jurassic source rocks,not just on the basis of tectonic disturbance and deep burial,but also from new studies in fluid inclusion measurements and the application of numerical simulation with EASY%Ro.Our study reveals the evolution process,tectonic episodes and the strength of the HG of the Jurassic source rock.We conclude that twice HG processes have taken place since the Lower Jurassic formation and infer from that the important conclusion that more HG of the Lower Jurassic source rock took place during the Eocene-Miocene epochs.Finally,we discuss the oil and gas tarp formation and destruction in the Lenghu tectonic belt and point out that more attention should be paid to the thrust faults,which formed during the late Himalayan epoch.
基金supported by the State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing(No.PRP/Open-1903)the Talents of Guizhou,China(Qian Ke He Platform and Talent(No.2017)5727-04)+1 种基金the Zunyi Normal University(No.BS[2018]04)the Qian Ke He Zhicheng(2018)2778.
文摘The Lenghu area is one of the most crucial tectonic belts for oil and gas exploration in the Qaidam Basin.However,reservoir distribution and the factors controlling petroleum accumulation in this area have not been studied in detail.In this paper,the structural characteristics and controlling factors of oil and gas accumulation in the Lenghu belt are investigated based on seismic profiles combined with drilling logs and microphotographs data.Results indicate that the Lenghu belt has thick source rocks and has preserved hydrocarbon generation conditions.Moreover,structural characteristics and lithology are the key factors controlling the reservoir distribution.The production of oil and gas layers are mainly distributed in high structural points and weak stress zones.The fracture zones and the weak stress zones are the potential places for the distribution of oil and gas reservoirs.
文摘冷湖地区因干旱少雨、晴天数多、云量覆盖少等特点,引起了天文学家的高度关注。2018年开始在冷湖赛什腾山开展光学视宁度测量,几年测量结果表明赛什腾山光学台址特性可比肩世界著名光学台址。为进一步了解赛什腾天文台址的电磁环境特性,开展了无人值守无线电干扰RFI(Radio Frequency Interference)测量设备的研制以及在赛什腾山天文台址的电磁环境监测。文章主要介绍基于研制的0.1~18 GHz频段RFI测量系统,在冷湖赛什腾山天文台址规划D点(海拔4055 m)开展为期超过一年的RFI测量,以及测量结果的评估。
