As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实例,我们重建了汤原断陷早第三纪期白垩系顶界三维古构造。
As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实例,我们重建了汤原断陷早第三纪期白垩系顶界三维古构造。
In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.
在国东部早第三纪沉积演化曾周期性发生海,形成了具有海相特征的岩石类型、古生物组合。
The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.
“盆”构造发育模式为:晚侏罗世到白垩纪末期发育的山间“盆”开始、发展到早第三纪断陷湖盆的发育、再演化为晚第三纪及第四纪陷发育阶段。
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