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系顶界三维古
。
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系顶界三维古
。
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”
育模式为:从晚侏罗世到
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。
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。
In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.
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
、
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”
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,我们重建汤原断陷早第三
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.
在中国东部早第三演化过程中曾周期性
发生过海侵,从而形成
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
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
白垩
末期发育的山间“盆
”开始、发展
断陷湖盆的发育、再演化为晚
及
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山间“
”
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纪中期白垩系顶界
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
白垩纪末期
育的山间“盆
”开始、
早
纪断陷湖盆的
育、再演化为晚
纪及
四纪
陷
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期白垩系顶界三维古构
。
In eastern China, transgression occured periodically during Eogene, and formed specially paleobio-cenosis,mineral association and rock type.
国东部早第三纪沉积演化过程
曾周期性
发生过海侵,从而形成了具有海相特征的岩
、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
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,
重建了汤原断陷早第三
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.
在中国东部早第三沉积演化过程中曾周
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
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
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
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
三纪断陷湖盆的发育、再演化为晚
三纪及
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,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。