位置：成果数据库 > 期刊 > 期刊详情页
Late Cretaceous paleomagnetic results from southeastern China, and their geological implication
  • ISSN号：0012-821X
  • 期刊名称：Earth and Planetary Science Letters
  • 时间：0
  • 页码：315-333
  • 语言：英文
  • 相关项目：华南武夷-诸广-武功地区加里东期构造作用和大陆动力学演化
作者： Yang, Zhenyu|Wang, Bin|
同期刊论文项目
华南武夷-诸广-武功地区加里东期构造作用和大陆动力学演化
期刊论文 67
同项目期刊论文
华南东段早古生代造山带研究
武夷山西缘流纹岩的形成时代及其地球化学特征
Structural development of the Lower Paleozoic belt of South China: Genesis of an intracontinental or
Components and episodic growth of Precambrian crust in the Cathaysia Block, South China: Evidence fr
江西付坊花岗岩体的年代学、地球化学特征及其成因研究
21世纪实验岩石学的重大突破——核幔边界D″层研究
华南东段前泥盆纪构造演化:来自碎屑锆石的证据
Geochemical features of Early Paleozoic granites in Jiangxi Province and their geological gnificance
武夷山地区前寒武纪地层沉积时代研究
锆石La-ICP-MS U-Pb与白云母40Ar/39Ar年代学及其对中国东南部早燕山事件的制约
Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of South China:
Pre-Devonian tectonic evolution of the eastern South China Block: Geochronological evidence from det
SHRIMP zircon U-Pb age, litho- and biostratigraphic analyses of the Huaiyu Domain in South China - E
Geochronological and geochemical features of the Cathaysia block (South China): new evidence for the
La-ICP-MS U-Pb and 40Ar/39Ar geochronology of the sheared metamorphic rocks in the Wuyishan：Constrai
Detrital zircon U-Pb geochronology, Hf-isotopes and geochemistry—New clues for the Precambrian crust
Study of geochemistry, geochronology and petro-genesis of the Early Paleozoic granitic plutons in th
华南早古生代花岗岩的地球化学、年代学及其成因研究－以赣中南为例
U-Pb Dating of Volcanic Rocks and Granites along the Wuyishan Belt: Constraints on Timing of Late Me
闽西南玮埔岩体和赣南菖蒲混合岩锆石La-ICPMS U-Pb年代学:对武夷山加里东运动时代的制约
Jurassic sedimentary features and tectonic settings of southeastern China
江西井冈山地区寒武-奥陶纪地层的Sm-Nd同位素组成及其构造意义
Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China
Paleoproterozoic basement beneath the southern Jiangxi Province: Evidence from U-Pb ages and Lu-Hf i
华南东段加里东期花岗岩类形成构造背景探讨
华南武功山地区韧性剪切带的纳米尺度测量研究
华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录
Geochemical characteristics of Early Paleozoic sedimentary rocks in the Jinggangshan area, Jiangxi p
Mesozoic tectonic evolution of the Southeast China Block: New insights from basin analysis
A comparative study of natural and experimental nano-sized grinding grain textures in rocks
岩石中纳米粒子层的观察厘定及其地质意义
Grenvillian orogeny in the Southern Cathaysia Block: Constraints from U-Pb ages and Lu-Hf isotopes i
Recent progress in studies on the nano-sized particle layer in rock shear planes
江西宁冈岩体的形成时代、地球化学特征及其构造意义
Late Palaeozoic-Early Mesozoic geological features of South China: Response to the Indosinian collis
Nano-texture of penetrative foliation in metamorphic rocks
Where was South China in the Rodinia supercontinent? Evidence from U-Pb geochronology and Hf isotope
岩石剪切面纳米粒子层的近期研究进展
花岗岩构造岩浆组合
Mesozoic-Cenozoic Basin features and evolution of Southeast China
Conglomeratic reservoir characterization in the Caiyu field of the Langgu sag, North China
Geochemistry and geochronology of the Fucheng Complex in the southeastern Jiangxi province, China
Formation age and origin of the Gutian-Xiaotao granitic complex in the southwestern Fujian province,
武夷山新元古代蛇绿混杂岩岩石地球化学特征
赣南存在古元古代基底：来自上犹陡水煌斑岩中捕虏锆石的U-Pb-Hf同位素证据
华夏南部可能存在Grenville期造山作用：来自基底变质岩中锆石U-Pb定年及Lu-Hf同位素信息
华夏地块显生宙的变质作用期次和特征
华南前泥盆纪构造演化：从华夏地块到加里东期造山带
南岭地区新元古代变质沉积岩的地球化学特征及构造意义
永安盆地晚古生代—中—新生代沉积构造环境演化特征
Paleoproterozoic basement beneath the southern Jiangxi Province： Evidence from U-Pb ages and Lu-Hf isotopes in zircons from the Doushui lamprophyre
Grenvillian oroseny in the Southern Cathaysia Block： Constraints from U-Pb ages and Lu-Hf isotopes in zircon from metamorphic basement
华南早中生代大地构造过程
锆石La-ICP-MS U-Pb与白云母~（40）Ar/~（39）Ar年代学及其对中国东南部早燕山事件的制约
闽西南玮埔岩体和赣南菖蒲混合岩锆石La—ICPMSU-Pb年代学：对武夷山加里东运动时代的制约
Sm-Nd isotopic compositions of Cambrian-Ordovician strata at the Jinggangshan area in Jiangxi Province： Tectonic implications
SHRIMP zircon U-Pb age, fitho- and biostratigraphic analyses of the Huaiyu Domain in South China,— Evidence for a Neoproterozoic orogen, not Late Paleozoic-Early Mesozoic collision