Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上岩体具有"平面分带、垂向分期、持续后退、继承性强"
分布特征。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上岩体具有"平面分带、垂向分期、持续后退、继承性强"
分布特征。
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.
“盆地”构造发育模式为:从晚侏罗到白垩
末期发育
山间“盆地”开始、发展到早
三
断陷湖盆
发育、再演化为晚
三
及
地陷发育阶段。
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观点;若发现问题,欢迎向我们指正。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"
分布特征。
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.
“盆地”构模式为:从晚侏罗
到白垩纪末期
间“盆地”开始、
展到早第三纪断陷湖盆
、再演化为晚第三纪及第四纪地陷
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观点;若
现问题,欢迎向我们指正。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"
分布特征。
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.
“盆地”构模式为:从晚侏罗
到白垩纪末期
间“盆地”开始、
展到早第三纪断陷湖盆
、再演化为晚第三纪及第四纪地陷
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观点;若
现问题,欢迎向我们指正。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上的砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"的分布特征。
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.
“盆地”构造发育模式为:从晚侏罗到白垩纪末期发育的山间“盆地”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地陷发育阶段。
声明:以上例句、词性分类联网资源自动生成,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。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖陡坡带上的砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"的分布特
。
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
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。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖陡坡带上的砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"的分布特征。
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.
“”
造发育模式为:从晚侏罗
到白垩纪末期发育的山
“
”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。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡上的砂砾岩体具有"平面分
、
分期、持续后退、继承性强"的分布特征。
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.
“盆地”构造发模式为:从晚侏罗
到白垩纪末期发
的山间“盆地”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地陷发
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,欢迎我们指正。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸陡坡带上的砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"的分布特征。
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.
“地”构造发育模式为:从晚侏罗
到白垩纪末期发育的山间“
地”开始、发
到早第三纪断陷
的发育、再演化为晚第三纪及第四纪地陷发育
。
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。
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸湖盆陡坡带上
砂砾岩体具有"平面
带、垂向
期、持续后退、继承性
"
布特征。
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.
“盆地”构造发育模式为:从晚侏罗白垩纪末期发育
山间“盆地”开始、发
第三纪断陷湖盆
发育、再演化为晚第三纪及第四纪地陷发育阶段。
声明:以上例句、词性类均由互联网资源自动生成,部
未经过人工审核,其表达内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。