Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆沉积,其中河流
、沼泽
泊
有规律
交替出现。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆沉积,其中河流
、沼泽
泊
有规律
交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在内堆积了从陆
到海
,从浅水到深水的各种
积体系,组成向上变细和变深的充填序列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆层序
层学方法对吐
侏罗系沉积层序进行了综合分析,划分出三套层序和一套超层序。
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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉积,其中河流相、沼泽相及湖泊相有规替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆内堆积了从陆相到海相,从浅水到深水的各种
积体系,组成向上变细和变深的充填序列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相序
方法对吐哈盆
侏罗系沉积
序进行了综合分析,划分出三套
序和一套超
序。
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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉,
河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆了从陆相到海相,从浅水到深水的各种
体系,组成向上变细和变深的充填
列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相地
学方法对吐哈盆地侏罗系沉
行了综合分析,划分出三套
和一套超
。
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,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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉积,其中河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆积了从陆相到海相,从浅水到深水的各种积体系,组成向
变细和变深的充填序列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相层序地层学方法对吐哈盆地侏罗系沉积层序进行了综合分析,划分出三套层序和一套超层序。
声:
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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉,
河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆了从陆相到海相,从浅水到深水的各种
体系,组成向上变细和变深的充填
列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相地
学方法对吐哈盆地侏罗系沉
行了综合分析,划分出三套
和一套超
。
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,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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉,
河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆了从陆相到海相,从浅水到深水的各种
体系,组成向上变细和变深的充填
列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相地
学方法对吐哈盆地侏罗系沉
行了综合分析,划分出三套
和一套超
。
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,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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西一
近海型的陆相沉积,其中河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆积了从陆相到海相,从浅水到深水的各种积体系,
成向上变细和变深的充填序列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相序地
学方法对吐哈盆地侏罗系沉积
序进行了综合分析,划分出
序和一
超
序。
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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一套近海型的陆相沉,其中河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆陆相到海相,
浅水到深水的各种
体系,组成向上变细和变深的充
。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相层地层学方法对吐哈盆地侏罗系沉
层
进行
综合分析,划分出三套层
和一套超层
。
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。
Shanxi Formation is a set of paralic continental deposit,of which,fluvial,swamp and lacustrine facies alternatively presented regularly.
山西组为一型的陆相沉积,其中河流相、沼泽相及湖泊相有规律地交替出现。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
在盆地内堆积了从陆相到相,从浅水到深水的各种
积体系,组成向上变细和变深的充填序列。
Nonmarine sequence stratigraphy is used to analyze Jurassic depositional sequences in Tu-ha basin, and three sequences and one supersequence are divided in this paper.
本文应用陆相层序地层学方法对吐哈盆地侏罗系沉积层序进行了综合,
出三
层序和一
超层序。
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的观点;若发现问题,欢迎向我们指正。