As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实,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。
As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实,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.
“”构造发育模式为:从晚侏罗世到白垩纪末期发育的
“
”开始、发展到早第三纪断陷湖
的发育、再演化为晚第三纪及第四纪
陷发育阶段。
声明:以上、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实例,我们汤原断陷早第三纪中期
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.
在中国东部早第三纪沉积演化过程中曾周期性发生过海侵,从而形成
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
纪末期发育的山间“盆
”开始、发展
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。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
As an example,the 3 D paleostructure of the boundary between Middle Eogene an...
作为实,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.
“”构造发育模式为:从晚侏罗世到白垩纪末期发育的
“
”开始、发展到早第三纪断陷湖
的发育、再演化为晚第三纪及第四纪
陷发育阶段。
声明:以上、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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中曾周期性
发生
海侵,
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
为晚第三纪及第四纪
陷发育阶段。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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
模式为:从晚侏罗世到白垩纪末期发
的山间“盆
”开始、发展到早第三纪断陷湖盆的发
、
化为晚第三纪及第四纪
陷发
阶段。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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:从晚侏罗世到白垩纪末期发育的山间“盆
”开始、发展到早第三纪
盆的发育、再演化为晚第三纪及第四纪
发育阶段。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我指正。
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纪中期白垩系
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的岩石类型、古生物
。
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.
“”构造发育模式为:从晚侏罗世到白垩纪末期发育的山间“
”开始、发展到早第
纪断陷湖
的发育、再演化为晚第
纪及第四纪
陷发育阶段。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
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期白垩系顶界三造。
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
过海侵,从而形成了具有海相特征的岩石类型、
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”
造发育模式为:从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。
声明:以上例句、词性分类均由互联网资源自动成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。