Cenozoic相关论文
Sclerophyllous evergreen broad-leaved forests,mainly made up of sclerophyllous oak,Quercus section Hetero-balanus (Φers......
Yunnan of southwestern China has long been well-known for high plant diversity.To understand the formation of this moder......
Carbonated source region for the Miocene mafic and ultra-mafic lavas from the western Qinling: impli
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During the early two decades of third millennium, many Mesozoic and Cenozoic biotas belong to plesiosaur, Titanosaurifor......
East Asian paleoclimate change in the Weihe Basin (central China) since the middle Eocene revealed b
Obtaining a continuous sedimentary record of Cenozoic East Asian paleoclimate change is key to understand the origin,evo......
Sedimentary Evolution of the Qinghai-Tibet Plateau in Cenozoic and its Response to the Uplift of the
We have studied the evolution of the tectonic lithofacies paleogeography of Paleocene Eocene,Oligocene,Miocene,and P......
Spinicaudatan clam shrimps are small and bivalved branchiopod crustaceans,which reached twice the acme of evolution ......
Cenozoic Crustally-derived Carbonate-rich Magmatic Rocks in West Junggar,North Xinjiang,Western Chin
The carbonate-rich magmatic rocks of West Junggar are distributed in the Baijiantan and Darbut ophiolitic mélanges in t......
Heavily populated by Beijing and Tianjin cities,Bohai basin is a seismically active Cenozoic basin suffering from huge l......
In the Korean Peninsula the Meso-Cenozoic basins were mainly formed due to fault block and block movement.The Mesozoic f......
Late Mesozoic-Cenozoic dcollement structure and its deep geological background in western Shandong,
Data from seismic reflection profiles, drilling, stratigraphy, structural deformation studies and physical rock properti......
Geological factors associated with unsuccessful exploration wells in the northern margin of the Qaid
We investigated the geological factors associated with unsuccessful exploration wells in the northern margin of the Qaid......
Structure and deformation around the Gyirong basin, north Himalaya, and onset of the south Tibetan d
Gyirong basin and its adjacent area are located at a special position in the Himalayan orogen, where the south Tibetan d......
Digital Simulation on Convergence Tendency between Southwest Tienshan and Pamirs-West Kunlun Systems
The collision between India plate and Eurasia continent 55 Ma ago caused the convergence between Southwest Tienshan and ......
Tectonic Framework and Deep Structure of South China and Their Constraint to Oil-Gas Field Distribut
South China could be divided into one stable craton,the Yangtze Craton (YzC),and several orogenic belts in the surroundi......
Layer-block tectonics of Cenozoic basements and formation of intra-plate basins in Nansha micro-plat
Layer-block tectonics (LBT) concept, with the core of pluralistic geodynamic outlook and multi- layer-sliding tectonic o......
This paper presents an overview of recent studies dealing with different ages of mantle peridotitic xenoliths and xenocr......
The mapping methods and division of tectonic units of the regional tectonic map in the eastern China
The geological-geophysical map series of the eastern China seas and adjacent region (1:1 000 000) will be published in t......
Tectonic diagenesis is a common and important geological phenomenon.We can fully understand the diagenesis of compressio......
Comparison of mantle-derived matierals from different spatiotemporal settings:Implications for destr
Cratonic destruction or lithospheric thinning beneath North China makes it as one of the most ideal areas for the studyi......
The helium and argon isotopic compositions of the ore-forming fluids from the molybdenum deposits such as Jinduicheng, D......
Features of Late Cenozoic Deepwater Sedimentation in Southern Qiongdongnan Basin, Northwestern South
Based on high resolution 2D and 3D seismic data acquired in recent years, using sequence stratigraphy analysis and geoph......
Cenozoic basalts are widely distributed in eastern China, and some of them contain zircon megacrysts which are considere......
介绍了北京西部地区新生代基岩的物理力学特性,并以穿越该地区的北京地铁9号线、14号线及轨道交通房山线建设过程中涉及到的新生代......
The Tengchong Cenozoic volcanic rocks belong to the high-K calc-alkaline rock series.They are strongly depleted in high ......
Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in t
On the basis of a newly-constructed record of magnetic susceptibility （SUS） and the depositional rate change of eolian loe......
Genesis of the Madang Cenozoic sodic alkaline basalt in the eastern margin of the Tibetan Plateau an
The Madang Cenozoic sodic alkaline basalt occurred in the eastern margin of the Tibetan Plateau, where is a key tectonic......
The Xunhua, Guide and Tongren Basins are linked with the Laji Mountain and the northern West Qinling thrust belts in the......
Geomorphological and environmental evolution in the upper reaches of the Yellow River during the lat
Studies of the geomorphology and stratigraphy in the upper reaches of the Yellow River during the late Cenozoic demonstr......
Late Cenozoic sedimentary process and its response to the slip history of the central Altyn Tagh fau
The ENE-striking Altyn Tagh fault (ATF), extending along the northern edge of the Tibetan Plateau, is one of the major i......
四集中高举时期，即， 60-35 ， 25-17 和 12-8 妈(但是在南部的西藏的喜马拉雅山脉的 18-13 妈)，并且后来，大约 5 妈，能被低温度的thermo年......
Our two newly obtained high-quality 40Ar/39Ar ages suggest that the high-K volcanic rocks of the Lawuxiang Formation in ......
The Weihe Basin,which is known as a Cenozoic rift Basin,is special for its location where not only enrich oil,gas and wa......
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Simulation of Ground Motion at Guanting Reservoir Dam Based on the Scenario Earthquake in the Yanqin
Research at home and abroad shows that the simulation of ground motion using the 3D finite-difference method might be ac......
Major and trace elements, REE concentrations and Sr, Nd isotope composihons have been measured in Bianmgou basaltic ande......
The method of determining the nitrogen isotopic composition of granites in the northeastern part of China is described. ......
Mechanisms of Cenozoic deformation in the Bohai Basin, Northeast China: Physical modelling and discu
The Bohai Basin is a Cenozoic petroliferous extensional basin in China and has apparent geometrical and kinematic simila......
Interpretation of new multichannel seismic reflection data from the Andaman Forearc Basin(AFB) in the northern Indian Oc......
TIANCHI volcano,Changbaishan Mountains isthe largest modern active volcano in East Chi-na.Many times strong volcanic er......
The chief Cenozoic formations of Kwangsi and Kwangtung have alreadybeen recognised and largely described,first by Richth......
The osmium isotopic compositions of Cenozoic basalts and peridotite xenoliths from Anhui and Jiangsu
THE determination of contents of trace (10~(-12)—10~(-9)) siderophile elements, Re and Os, and osmium isotopic composi......
The Late Cenozoic stratigraphic sequence and its information of tectonic evolution are obtained here through the detaile......
Integrated fission track and (U-Th)/He analysis is carried out on 6 apatite and 6 zircon samples from a near vertical se......
40Ar/39Ar ages were determined for 6 phlogopite samples from a kamafugite pipe occurring in western Qinling, yielding a ......
Mesozoic subduction-accretion zone in northeastern South China Sea inferred from geophysical interpr
A segment of Mesozoic subduction-accretion zone was inferred across the northeastern South China Sea at approximately NE......
Petrography and Geochemistry of Peridotite Xenoliths from Hannuoba and Significance for Lithospheric
The compositions of the whole rocks and trace elements of minerals in peridotites can reflect the characteristics of the......
In this study, from the travel time data recorded in the Tianshan passive seismic array experiment, we present the P-wav......
The thickness and structural characteristics of the crust across Tibetan plateau from active-sources
The Tibetan plateau as one of the youngest orogen on the Earth was considered as the result of continent-continent colli......
