PALEOENVIRONMENT相关论文
,Geochemical record for the depositional condition and petroleum potential of the Late Cretaceous Ma
Carbonaceous shale exposures of the Late Cretaceous Mamu Formation along Ifon-Uzebba road in weste arm (Benin Flank) of ......
Palynomorphs in the first paleosol layer in the Yangtze Delta and their paleoenvironmental implicati
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......
Research on the Effects of the Contents of Radioactive Elements on Granularity and Climate Change: A
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......
Elemental characteristics and paleoenvironment reconstruction:a case study of the Triassic lacustrin
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......
Oceanic environmental changes of subarctic Bering Sea in recent 100 years: Evidence from molecular f
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......
Occurrences of warm-adapted mammals in north China over the Quaternary Period and their paleo-enviro
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......
Phase Evolution of Holocene Paleoenvironmental Changes in the Southern Yellow Sea: Benthic Foraminif
Assemblages of benthic foraminifera in a sediment core(C02)near the western margin of the southern Yellow Sea Mud were s......
δ13CSC values of the loess-paleosol sequence in Dali area, Shaanxi Province, China, and paleoenviron
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......
Formation and Evolution of a Paleosol across the Lower Silurian-Lower Permian Boundary in Zunyi Dist
This paper presents a set of bulk geochemical and mineralogical data from a paleoweathering profile located in Zunyi Dis......
Microconchids from Microbialites near the Permian-Triassic Boundary in the Zuodeng Section, Baise Ar
Abundant microconchid worm tubes were extracted from the microbialites deposit near the Permian-Triassic boundary at the......
涌潮是在涨潮过程中潮波向上游方向行进的水跃现象,广泛存在于潮差大、平面上呈喇叭状的河口地区.研究涌潮沉积对了解河口湾区域的......
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 Primary Observation on Palynofacies of the Chuangde Section (Late Jurassic-Cretaceous), Gyangzê, S
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......
Paleoenvironmental Evolution of the Beilun River Estuary, Northwest South China Sea, During the Past
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......
Occurrence of Middle Miocene Fossil Cyprinid Fish in the Northern Qaidam Basin and its Paleoenvironm
With a thick sequence of early Eocene to Pleistocene terrestrial records, the Qaidam Basin on the northern Tibetan Plate......
含火山灰层沉积的植硅体分析为了解植被对从空中下降的火山灰的反应提供新的信息.新西兰霍克湾的一个深197m钻孔的上部50 m样品,提......
This paper reports different concentration patterns of n-alkanes distribution in the sediments from the Chukchi Sea, the......
We studied the records of elemental carbon (EC) of the last 21 ka in the Weinan loess section, Shanxi Province. The vari......
Middle Ordovician Bioturbation Structures from Southeastern Margin of Ordos Basin and Their Environm
Trace fossils were discovered in the Middle Ordovician Badou Member of Fengfeng Formation and the Member 1 of Jinsushan ......
In recent decades, environmental magnetism has become an important method for studying past global climatic and environm......
δ13CSC values of the loess-paleosol sequence in Dali area, Shaanxi Province, China, and paleoenviron
The carbon isotopic ratios of carbonate in the two profiles of the Dali area were analyzed and some new understandings o......
Based on detailed measurement in the field and a comPrehensive analysis of carbonate microfacies, the Pennsylvanian reef......
Paleontologists search the fossil record for evidence of age, ancient environments, phylogenetic reconstructions and anc......
Oceanic environmental changes of subarctic Bering Sea in recent 100 years: Evidence from molecular f
The core sample B2-9 from the seafloor of the subarctic Bering Sea was dated with 210Pb to obtain a consecutive sequence......
