We report new material of the zalambdalestid,Zhangolestes jilinensis,from the Quantou Formation(lower Upper Cretaceous,Cenomanian to Turonian),Gongzhuling City,Jilin Province,NE China.Using micro-CT-scan,the material ...We report new material of the zalambdalestid,Zhangolestes jilinensis,from the Quantou Formation(lower Upper Cretaceous,Cenomanian to Turonian),Gongzhuling City,Jilin Province,NE China.Using micro-CT-scan,the material is shown to include dentocranial and postcranial elements recovered from the same matrix block containing the holotype specimen.The CT-images also show the labial and internal structures of the holotype fragment of the lower jaw of Z.jilinensis.Based on the preservation,relative size,and tooth wear,the new material and the holotype lower jaw likely belong to the same individual animal,whereas the hypodigm mandibular fragment assigned to Z.jilinensis in the original study is thought now to belong to a different individual,potentially representing a different species,which,if true,would increase the eutherian diversity in the Late Cretaceous Changchunsaurus Fauna.Furthermore,the new CT-images show that the incisor morphology is diverse within zalambdalestids and probably evolved independently from the enlarged incisors in placental mammals,such as Glires.展开更多
Based on the geochemical,seismic,logging and drilling data,the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics...Based on the geochemical,seismic,logging and drilling data,the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics,the tight oil enrichment model and its major controlling factors.First,the Quantou Formation is overlaid by high-quality source rocks of the Upper Cretaceous Qingshankou Formation,with the development of nose structure around sag and the broad and continuous distribution of sand bodies.The reservoirs are tight on the whole.Second,the configuration of multiple elements,such as high-quality source rocks,reservoir rocks,fault,overpressure and structure,controls the tight oil enrichment in the Fuyu reservoirs.The source-reservoir combination controls the tight oil distribution pattern.The pressure difference between source and reservoir drives the charging of tight oil.The fault-sandbody transport system determines the migration and accumulation of oil and gas.The positive structure is the favorable place for tight oil enrichment,and the fault-horst zone is the key part of syncline area for tight oil exploration.Third,based on the source-reservoir relationship,transport mode,accumulation dynamics and other elements,three tight oil enrichment models are recognized in the Fuyu reservoirs:(1)vertical or lateral migration of hydrocarbon from source rocks to adjacent reservoir rocks,that is,driven by overpressure,hydrocarbon generated is migrated vertically or laterally to and accumulates in the adjacent reservoir rocks;(2)transport of hydrocarbon through faults between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downward through faults to the sandbodies that are separated from the source rocks;and(3)migration of hydrocarbon through faults and sandbodies between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downwards through faults to the reservoir rocks that are separated from the source rocks,and then migrates laterally through sandbodies.Fourth,the differences in oil source conditions,charging drive,fault distribution,sandbody and reservoir physical properties cause the differential enrichment of tight oil in the Fuyu reservoirs.Comprehensive analysis suggests that the Fuyu reservoir in the Qijia-Gulong Sag has good conditions for tight oil enrichment and has been less explored,and it is an important new zone for tight oil exploration in the future.展开更多
基金supported by the National Natural Science Foundation of China(Grant Nos.42122010,42072017)the Youth Innovation Promotion Association CAS(Y2023017)+1 种基金the National Mineral Rock and Fossil Specimens Resource Center(NCSTI-RMF20240203)China Geological Survey(DD20230221)。
文摘We report new material of the zalambdalestid,Zhangolestes jilinensis,from the Quantou Formation(lower Upper Cretaceous,Cenomanian to Turonian),Gongzhuling City,Jilin Province,NE China.Using micro-CT-scan,the material is shown to include dentocranial and postcranial elements recovered from the same matrix block containing the holotype specimen.The CT-images also show the labial and internal structures of the holotype fragment of the lower jaw of Z.jilinensis.Based on the preservation,relative size,and tooth wear,the new material and the holotype lower jaw likely belong to the same individual animal,whereas the hypodigm mandibular fragment assigned to Z.jilinensis in the original study is thought now to belong to a different individual,potentially representing a different species,which,if true,would increase the eutherian diversity in the Late Cretaceous Changchunsaurus Fauna.Furthermore,the new CT-images show that the incisor morphology is diverse within zalambdalestids and probably evolved independently from the enlarged incisors in placental mammals,such as Glires.
基金Supported by the PetroChina Science and Technology Major Project(2016E0201)。
文摘Based on the geochemical,seismic,logging and drilling data,the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics,the tight oil enrichment model and its major controlling factors.First,the Quantou Formation is overlaid by high-quality source rocks of the Upper Cretaceous Qingshankou Formation,with the development of nose structure around sag and the broad and continuous distribution of sand bodies.The reservoirs are tight on the whole.Second,the configuration of multiple elements,such as high-quality source rocks,reservoir rocks,fault,overpressure and structure,controls the tight oil enrichment in the Fuyu reservoirs.The source-reservoir combination controls the tight oil distribution pattern.The pressure difference between source and reservoir drives the charging of tight oil.The fault-sandbody transport system determines the migration and accumulation of oil and gas.The positive structure is the favorable place for tight oil enrichment,and the fault-horst zone is the key part of syncline area for tight oil exploration.Third,based on the source-reservoir relationship,transport mode,accumulation dynamics and other elements,three tight oil enrichment models are recognized in the Fuyu reservoirs:(1)vertical or lateral migration of hydrocarbon from source rocks to adjacent reservoir rocks,that is,driven by overpressure,hydrocarbon generated is migrated vertically or laterally to and accumulates in the adjacent reservoir rocks;(2)transport of hydrocarbon through faults between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downward through faults to the sandbodies that are separated from the source rocks;and(3)migration of hydrocarbon through faults and sandbodies between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downwards through faults to the reservoir rocks that are separated from the source rocks,and then migrates laterally through sandbodies.Fourth,the differences in oil source conditions,charging drive,fault distribution,sandbody and reservoir physical properties cause the differential enrichment of tight oil in the Fuyu reservoirs.Comprehensive analysis suggests that the Fuyu reservoir in the Qijia-Gulong Sag has good conditions for tight oil enrichment and has been less explored,and it is an important new zone for tight oil exploration in the future.
