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
、
及湖泊
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
、
及湖泊
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.
在盆内堆积了从陆
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
层学方法对吐哈盆
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.
在盆地内堆积了从相到海相,从浅水到深水
各种
积体系,组成向上变细和变深
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.
本文应用相层序地层学方法对吐哈盆地侏罗系沉积层序进行了
析,划
出三套层序和一套超层序。
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
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沉积,其中河流
、沼泽
及湖泊
有规律地交
。
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
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.
本文应用陆地
学方法对吐哈盆地侏罗系沉积
进行了综合分析,划分
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,其表达内容亦不代表本软件的观点;若发问题,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
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.
本文应用陆相学方法对吐哈盆
侏罗系沉积
进行了综合分析,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,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海相,从
深
的各种
积体系,组成
细和
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。
声明:以例句、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。
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
及
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.
本文应用陆层序地层学方法
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律出现。
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
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.
本文应用陆相学方法对吐哈盆
侏罗系沉积
进行了综合分析,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,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.
在盆地内堆积了陆相到海相,
到深
的各种
积体系,组成向
和
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。
声明:以例句、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沉积,其中河流
、沼泽
及湖泊
有规律地交替出
。
These basins were generally filled with upward fining and deepening sedimentary sequence that comprises nonmarine to marine, shallow marine to deep marine depositional systems.
地内堆积了从
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.
本文应层序地层学方法对吐哈
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;若发问题,欢迎向我们指正。