Cretaceous granites form a northerly trending belt.
白垩花岗岩的分布
向北延伸。
Cretaceous granites form a northerly trending belt.
白垩花岗岩的分布
向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩典型的“温室”气候和海洋一直是地学界关注的焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩的隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到白垩末期发育的山间“盆地”开始、发展到早
断陷湖盆的发育、再演化为晚
及
四
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,其表内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩纪花岗岩分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩纪典型“
”
候和海洋一直是地学界关注
焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩纪隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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”构造模式为:从晚侏罗世到白垩纪末期
山间“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,其表内容亦不代表本软件
观点;若
现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
垩纪花岗岩的分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
垩纪典型的“温室”气候和海洋
地学界关注的焦点之
。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了垩纪的隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散
其中地区域。
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:从晚侏罗垩纪末期发育的山间“盆地”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,其表内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
纪花岗岩的分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
纪典型的“温室”气候和海洋一直是地学界关注的焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了纪的隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到纪末期发育的山间“盆地”开始、发展到早第三纪断陷湖盆的发育、
为晚第三纪及第四纪地陷发育阶段。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩纪花岗布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩纪典型“温室”气候和海洋一直是地学界关注
焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩纪隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到白垩纪末期发育
山间“
地”开始、发展到早第三纪断
发育、再演化为晚第三纪及第四纪地
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
内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
纪花岗岩的分布呈带状向北延
。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
纪典型的“温室”气候和海洋一直是地学界关注的焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了纪的隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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”构造育模式为:从晚侏罗世到
纪末期
育的山间“盆地”
、
展到早第三纪断陷湖盆的
育、再演化为晚第三纪及第四纪地陷
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,其表内容亦不代表本软件的观点;若
现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩纪花分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩纪典型“温室”气候和海洋一直是地学界关注
焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩纪隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到白垩纪末期发育
山间“
地”开始、发展到早第三纪断陷
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、词性分类均由互联网资源自动生成,部分未经过人工审核,其表内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩纪花岗岩的分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩纪典型的“温室”气候和海洋一直是地学界关注的焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩纪的隔离,接着特有马
散布及随后从马
扩散到其中地区域。
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:从晚侏罗世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、词性分类均由互联网资源自动生成,部分未经过人工审核,其表内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩花岗岩的分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩典型的“温室”气候和海洋一直是地学界关注的焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩的隔离,接着特有种在马
加斯加听散布
随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到白垩末期发育的山间“盆地”开始、发展到早
三
断陷湖盆的发育、再演化为晚
三
四
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,其表内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Cretaceous granites form a northerly trending belt.
白垩纪花岗岩分布呈带状向北延伸。
Abstract :The Cretaceous greenhouse climate and paleoceanography is one of hot topics in the Earth sciences during the past twenty years.
白垩纪典“温室”气候和海洋一直是地学界关注
焦点之一。
In both cases, the researchers have evoked scenarios of Cretaceous vicariance, followed by endemic species radiation within Madagascar and subsequent dispersal from Madagascar to other areas.
这些情形,研究人员已经考虑了白垩纪隔离,接着特有种在马
加斯加听散布及随后从马
加斯加扩散到其中地区域。
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:从晚侏罗世到白垩纪末期发育
“
地”开始、发展到早第三纪断陷湖
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、词性分类均由互联网资源自动生成,部分未经过人工审核,其表内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。