As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我了汤原断陷早第三中期系顶界三维古构造。

In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.

在中国东部早第三沉积演化过程中曾周期性发生过海侵,从而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：从晚侏罗世到末期发育的山间“盆”开始、发展到早第三断陷湖盆的发育、再演化为晚第三及第四陷发育阶段。

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中期白垩系顶界维古构造。

In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.

在中国东部早沉积演化过程中曾周期性生过海侵,从而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”构造育模式为：从晚侏罗世到白垩末期育的山间“盆”开、到早断陷湖盆的育、再演化为晚及四陷育阶段。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

实例，我们重建了汤原断陷早第三纪中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.

在中国东部早第三纪沉积演化过程中曾周期性发生过海侵,从而形成了具有海相特征岩石类型、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”构造发模式：从晚侏罗世到白垩纪末期发间“盆”开始、发展到早第三纪断陷湖盆发、再演化晚第三纪及第四纪陷发阶段。

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。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作，我们重建了汤原断陷早第三纪中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.

在中国东部早第三纪沉积演化过程中曾周性生过海侵,从而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”构造模式：从晚侏罗世到白垩纪末的山间“盆”开始、展到早第三纪断陷湖盆的、再演化晚第三纪及第四纪陷阶段。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

例，我们重建了汤原断陷早第三纪中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.

在中国东部早第三纪沉积演化过程中曾周期性生过海侵,从而形成了具有海相特征岩石类型、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”构造模式：从晚侏罗世到白垩纪末期山间“盆”开始、展到早第三纪断陷湖盆、再演化晚第三纪及第四纪陷阶段。

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中期白垩系顶界维古构造。

In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.

在中国东部早沉积演化过程中曾周期性发生过侵,从而形成了具有特征的岩石类型、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：从晚侏罗世到白垩末期发育的山间“盆”开始、发展到早断陷湖盆的发育、再演化为晚及四陷发育阶段。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作实例，我们重建了汤原断三纪中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.

在中国东部三纪沉积演化过程中曾周期性发生过海侵,而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：侏罗世到白垩纪末期发育的山间“盆”开始、发展到三纪断湖盆的发育、再演化三纪及四纪发育阶段。

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中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.

在中国东部早第三纪沉积演化程中曾海侵,从而形成了具有海相特征的岩石类型、古物组合。

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”构造育模式为：从晚侏罗世到白垩纪末育的山间“盆”开始、展到早第三纪断陷湖盆的育、再演化为晚第三纪及第四纪陷育阶段。