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alluvial deposit相关的网络例句

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According to the characters of organic maceral, organic type, biomarker,it can be divided to five types of sedimentary facies: unrest restricted sea graptolite facies, alluvial restricted sea, carbonate mesa algal deposit facies, mud mesa algal deposit facies and deep water shelf algal deposit facies.

根据烃源岩有机显微组分、有机质类型、生物标志物及成烃能力等特征划分出五类沉积有机相,即动荡局限海笔石相、滞流局限海笔石相、碳酸盐台地藻积相、泥质台地藻积相和深水陆棚藻积相。

As the lake basin shoals and silts up, the color of clastic sediment gradually changes from black, black gray, gray and grayish green to purplish grey and red purple, meaning that the subaerial alluvial fan deposit of late stage has replaced the fan-delta deposit and that the coal-forming process ends.

待湖盆逐渐变浅和淤积,碎屑沉积物的颜色由黑、黑灰、灰、灰绿逐渐变为紫灰和紫红,表明晚期陆上冲积扇沉积已经代替了扇三角洲沉积,成煤作用随之结束。

The sense "alluvial deposit" is not recorded until 1555, when delta is used with reference to the Nile River delta.

&淤积沉淀&这个含义直到1555年才有记载,那时delta 被用于特指尼罗河口的三角洲

Lake deposit Facies analysis Alluvial fan Underwater fan Delta Reservoir Sedimentary mode Channel deposit

湖泊沉积;相分析;冲积扇;水下扇;三角洲;储集层;沉积模式;河道沉积

And the lower yellow loam is the alluvial deposit of the ancient yellow river.

下部黄色壤土层系古黄河冲洪积沉积物。

After the investigation and study on Alluvial Tin deposit in Changning Dayishan Mine,Conclude that its geologic setting mainly iles in its structure and land form a proper scale of Alluvial Tin deposit were found in the limestone solution cave around Dayishan granite body.

提出了在大义山花岗岩体外围灰岩溶洞发现了一定规模的砂锡矿床,并初步分析了形成原因。

The sedimentary environment divided in to fluvial deposit and lacustrine deposit. The sedimentary evolution of each depositional circle usually began with alluvial channel to fluvial deposit, and evolved into lacustrine deposit which is mainly made up of shore-shallow lake sedimentary model with relatively stirring hydrodynamic condition.

其沉积环境主要可以分为河流沉积和湖泊沉积两种类型,每一个沉积旋回都是以洪积扇到河流相沉积开始,向湖泊相沉积演化,湖泊沉积阶段主要以湖水相时动荡的滨浅湖沉积为主。

The study results show that:①The distribution of Cd in shallow surface soils is characterized as: The content of Cd in lacustrine deposit, alluvial lacustrine and alluvial-diluvial low-lying plain is 1.4 to 1.8 times as high as in alluvial-diluvial high valley flat and alluvial-diluvial high bank physiognomy areas.②The content variation of Cd in horizontal distribution was controlled by clay primarily and OrgC secondly. The variation of OrgC was major factor that affected the content variation of Cd in vertical distribution.

结果表明:①研究区浅层土壤中w的分布特征为,湖积低平原区、冲-湖积低平原区及冲洪积低洼平原区地貌成因类型土壤中的含量明显高于冲洪积高漫滩平原区、冲洪积高亢平原区地貌成因类型土壤,其质量分数差异达1.4~1.8倍;②研究区不同地貌成因类型土壤中,w的横向分布特征主要受黏粒含量分布的控制,其次是wC(下标 org;垂向分布特征的主要控制因素是wC

The sedimentary environment divided into fluvial deposit and lacustrine deposit. The sedimentary evolution of each depositional circle usually began with alluvial channel to fluvial deposit, and evolved into lacustrine deposit which is mainly made up of shore-shallow lake sedimentary model with relatively stirring hydrodynamic condition.

其沉积环境主要可以分为河流沉积和湖泊沉积两种类型,每一个沉积旋回都是以洪积扇到河流相沉积开始,向湖泊相沉积演化,湖泊沉积阶段主要以湖水相对动荡的滨浅湖沉积为主。

The investigation and study of seismic hazard in frozen soils deposit region by the West of Kunlun mountain pass M 8.1 earthquake in 2001 shows that there is frozen soils distribution in the region, which mainly result from the glacial deposit, alluvial deposits, deluvial deposits, lacustrine deposits, and of which the depth varies greatly along the rupture.

通过对2001年昆仑山口西8.1级地震区冻土震害考察研究表明,震区主要存在冰碛、冲积、洪积和湖积等成因的冻土,沿地震破裂带冻土厚度变化较大。

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