1) Early Jurassic strata
早侏罗世地层
1.
Early Jurassic strata and sporopollen assemblagesin the northern Hami depression,Xinjiang;
新疆哈密拗陷北部早侏罗世地层及其孢粉组合
2) Lower Jurassic
早侏罗世<地>
3) Early Jurassic epoch
早侏罗世
1.
Through analyzing the sedimentary environment properties in Sichuan Basin during Da anzai Age of Early Jurassic Epoch,a theoretical model of lake basin sequence in Da anzai Age is set up,the actual sedimentary sequence properties of Da anzai Formation are discussed and then the sequence units are further divided in the paper.
通过分析早侏罗世大安寨期四川盆地的环境特征 ,建立了大安寨期湖盆层序的理论模型 ,并对大安寨组实际沉积层序特征进行了探讨 ,进而对层序单元作了进一步的划分。
4) Early Jurassic
早侏罗世
1.
Early Jurassic Zircon SHRIMP U-Pb Age of the Dacitic Volcanic Rocks in the Southeastern Zhejiang Province Determined Firstly and Its Geological Significances;
浙东南英安质火山岩早侏罗世锆石SHRIMP年龄的首获及其地质意义
2.
Late Triassic and Early Jurassic Ammonoids from Eastern Himalayas;
东喜马拉雅地区晚三叠世—早侏罗世的菊石类
3.
Early Jurassic sporopollen assemblages from the Toksun subbasin in the Turpan-Hami basin, Xinjiang and their significance;
新疆吐鲁番——哈密盆地托克逊凹陷早侏罗世孢粉植物群及其意义
5) Lower Jurassic
早侏罗世
1.
By a comprehensive comparison of its basic characteristics, it is believed that it was formed during late Triassic epoch-lower Jurassic, about 213~192 Ma.
清溪超单元成岩年代历有争议 ,笔者在该区从事 1∶5万区域地质调查时 ,从野外地质特征、岩石学、岩石化学、同位素年代学等方面的特征对该超单元进行了系统的调查取样 ,综合类比其基本特征 ,认为其成岩年代应属晚三叠世—早侏罗世 ,成岩时限约在 2 13~ 192M
6) early-middle Jurassic
早中侏罗世
1.
Sedimentary Characteristics and Model of Early-Middle Jurassic in Jiyang Depression;
济阳坳陷早中侏罗世沉积特征与沉积模式
2.
Synthetically analyzed the fracture, earthquake, coal ranks and their distribution, coal seam抯 buried depth and so on, the authors have realised that low-rank bituminites, early-middle Jurassic in Tianshan area, are formed by burial metamorphism, and it is widespread.
通过对天山地区的断裂构造、地震、地热、煤级及其时空分布、煤层埋深等因素的综合分析,认为天山北缘及其邻区早中侏罗世大范围分布的低级烟煤主要由深成变质作用形成,深成变质作用具普遍性。
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