biostratigraphy相关论文
Age of the earliest transgressive event in the Krishna-Godavari Basin, India:evidence from dinoflage
A combined biostratigraphic study of dinoflagellate cysts and foraminifera was carried out on Early Cretaceous subsurfac......
New Findings of Latest Early Olenekian (Early Triassic) Fossils in South Primorye, Russian Far East,
Information on latest early Olenekian (latest Smithian) ammonoids is available apparently from only seven regions of the......
对新疆维吾尔自治区沙湾县玛纳斯河红沟侏罗系剖面开展了生物地层学、同位素年代地层学、旋回地层学和磁性地层学等的综合研究。研......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Foraminiferal biostratigraphy of lignite mines of Kutch, India: Age of lignite and fossil vertebrate
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Calcareous nannoplankton dating of the Late Quaternary deposits in Greece and the eastern Mediterran
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Conodonts from the Sesong Slate and Hwajeol Formation (Guzhangian to Furongian) in the Taebaeksan Ba
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Reexamination of Radiolarian Biostratigraphy in Permian in Pelagic Chert Sequences at Dachongling Se
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Di
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
A Middle-Upper Devonian Boundary Section in the Open Platform, Platform Margin Facies of Guilin,Sout
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Conodont Biostratigraphy and Age Determination of the Lower-Middle Triassic Boundary in South Guizho
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Trilobite Biostratigraphy of the lower Paleozoic (Cambrian-Ordovician) Joseon Supergroup, Taebaeksan
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Scleractinian corals appeared during the Anisian period of the Triassic after the end-Permian mass extinction, which in ......
Larger Foraminiferal Biostratigraphy and Facies Analysis of the Oligocene-Miocene Asmari Formation i
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
The Cretaceous of Afghanistan is marked by great facies diversity. The evolution of Cretaceous basins is part of a comp......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
The genus Ovatoryctocara Tchernysheva,1962,and its key species Ovatoryctocara granulata Tchernysheva,1962,are revised. O......
Conodont Biostratigraphy and Age Determination of the Lower-Middle Triassic Boundary in South Guizho
The demarcation of the Lower-Middle Triassic boundary is a disputed problem in global stratigraphic research. Lower-Midd......
The aim of this study is to discuss the chronostratigraphy, catastrophic event stratigraphy, biostratigraphy and sequenc......
A biostratigraphic study of calcareous nannofossils of sediments from Lingfeng No. 1 well in the East China Sea was carr......
On the basis of the faunas including conodonts Palmatolepis gracilis sigmoidalis, P.gracilis gracilis, Polygnathus germa......
With abundant deep-water upper Permian sediments, Guizhou is an ideal place for the research of radiolarian biostratigra......
藏南定日遮普惹山剖面主要是Albian晚期到古近纪海相沉积,Willems等(1996)对岩石地层和沉积微相进行了详细研究,并通过浮游有孔虫......
Study on a Terrestrial Permian-Triassic Boundary Section-Zhejue Section, Weining County, Guizhou Pro
The Zhejue Section is an excellent terrestrial Permian-Triassic boundary (TPTB) section not only for its convenient acce......
Reexamination of Radiolarian Biostratigraphy in Permian in Pelagic Chert Sequences at Dachongling Se
Permian radiolarian biostratigraphy was reexamined in the bedded chert section in Qinzhou area of southeast Guangxi Zhua......
本研究利用保存丰富、完好的放射虫对塔斯曼海更新世层序进行地层学分析.对塔斯曼海南部更新世的KH94-4TSP-4PC岩芯的放射虫组合进......
The Khami group within the petroliferous Zagros Basin of Iran includes the Surmeh, Hith, Fahliyan, Gadvan and Dariyan fo......
由于地处低纬度下扬子碳酸盐缓坡台地较深水区,安徽巢湖地区的下三叠统由一系列泥、灰岩旋回层组成,并含有丰富的菊石化石.通过对......
