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信江盆地
    The Shixi Formation in the Xinjiang Basin of Jiangxi and its biota and age
    江西信江盆地石溪组生物群及其时代
    LATE EARLY CRETACEOUS CHAROPHYTES FROM THE XINJIANG BASIN,JIANGXI AND THEIR STRATIGRAPHIC SIGNIFICANCE
    江西信江盆地早白垩世晚期轮藻及其地层意义
    Study on Late Mesozoic Structural Evolution in Xinjiang Basin, Northeast Jiangxi Province
    赣东北信江盆地中生代晚期构造演化研究
    Fossil of Coelurosauria in the Xinjiang basin, northeastern Jiangxi
    赣东北信江盆地的虚骨龙类化石
    THE JURASSIC-CRETACEOUS BOUNDARY BASED ON NEW DATA FROM THE XINJIANG BASIN
    从信江盆地新资料论侏罗、白垩系的界线
    OSTRACODS FROM THE UPPER PART OF ZHOUJIADIAN FORMATION,XINJIANG BASIN, JIANGXI
    江西信江盆地周家店组的介形类化石
    REGIONAL GOLOGICAL TECTONICS AND METALLIZATION OF XINJIANG BASIN,JIANGXI
    江西信江盆地区域地质构造与成矿作用
    THE GEOCHEMICAL CHARACTERISTICS OF CHERTS IN THE CARBONIFEROUS PERIOD AND THEIR SENDIMENTARY ENVIRONMENT IMPLICATIONS IN XINJIANG BASIN
    信江盆地石炭纪硅质岩地球化学特征及沉积环境意义
    Late Cretaceous eolian dunes and wind directions in Xinjiang basin, Jiangxi Province, China
    江西信江盆地晚白垩世风成沙丘的发现及其古风向
    They have all ofcertain characteristics of hydrothermal sediment cherts.  Finally, the ratioes of MnO/TiO2, the values of δCe and δ30Si show that the sedimentary environment of the cherts in Xinjiang basin was chiefly the epeiric sea in continental margin. 
    由硅质岩MnO/TiO2比值、δCe值和δ30Si值分析表明,信江盆地石炭纪硅质岩的沉积环境主要为浅海。
    sing the information of remote sensing and combining with the sedimentary formation analysis to pick out and study chronostratigraphic interface in cretaceous period basin in the course of studying intracontinental deformation evolution about North-eastern Jiangxi Jiangnan orognic belt and filling sequence of Xinjiang basin.
    笔者在进行赣东北江南造山带印支—燕山碰撞造山后陆内变形演化与信江盆地充填系列研究中,利用TM遥感图像影像信息结合沉积建造分析,对白垩纪盆地中等时性地层界面进行识别与研究。
    In the course of mapping in shangrao area, the late Mesozoic structural evolution stage in Xinjiang basin, northeast Jiangxi province can be divided into intracontinental collision orogen in early stage of Yanshan and intracontinental rift age, sag age, inversion age in middle late stage of Yanshan two stages based on the information of magmatic activity, analysis of depositional system and deep structure. The main period of structural conversion is early stage and early middle stage in early cretaceous
    在江西上饶地区填图当中,基于岩浆活动、沉积体系分析和地貌景观及深部构造等信息,本文提出了赣东北信江盆地中生代晚期构造演化,可划分为:早燕山陆内碰撞造山和中晚燕山陆内裂谷期、坳陷期及反转期两个阶段,主要构造转换的时间在早白垩世早期与早中期的认识。
    The Tangbian Formation (K2t), middle part of the Late Cretaceous Guifeng Group in Xinjiang Basin, Jiangxi Province, has long been thought to be aqueous.
    长期以来,江西信江盆地晚白垩世圭峰群塘边组(K2t)均定为水成沉积,本文的研究结果则认为属风成沉积。
 

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