At the same time, the four different genesis types of the sequence interfaces are divided: orogenic erosive sequence unconformity interface, uplift erosive sequence unconformity interface, transgression onlap sequence unconformity interface, exposural sequence unconformity interface; simultaneously the ten concrete mineral showing forms are summarized, i.e. paleo-weathering crust, drossy layer, river rejuvenation surface, paleo-karst surface, slope gravity current erosion surface, intrabasin turbid flow erosion surface, volcanic events surface, lithologic and lithofacies conversion surface, onlap surface and maximium sea flooding surface.

同時歸納出了4種不同的層序界面成因類型：造山侵蝕層序不整合界面AVwww在线观看、升隆侵蝕層序不整合界面、海侵上超層序不整合界面和暴露層序不整合界面等自拍亚洲国产；同時總結(jié)出10種具體的物質(zhì)表現(xiàn)形式久章草在线精品视频欧美九狼，即：古風(fēng)化殼、渣狀層一级毛片无码不卡直接观看、河流回春作用面美女赤裸露私密部位网站、古喀斯特作用面、斜坡重力流沖刷侵蝕面久艹自拍偷拍、盆地內(nèi)濁流侵蝕面国产欧美色,一区二区三区、火山事件作用面、巖性AV天堂永久网、巖相轉(zhuǎn)換面亚洲va国产日韩欧美精品色婷婷、上超面和最大海泛面。

The results indicate that the tempestite in the area has lots of rock types including clastic rocks, bioclastic limestones and volcaniclastic rocks. The cumulative probability plots have "high slope-multi-bouncing population-1 suspension population" pattern, multi segments pattern and "high slope 1 segment" pattern. The sedimentary structures include gutter cast, surface of scour, cut structure, graded bed, massive bedding, hummocky cross stratification, parallel bedding, ripples, contemporaneous deformation and Fugichnia. The grains distribution and sedimentary structures shier that the transportation medium is characterized by tractive current and gravity flow synchronously.

結(jié)果表明性爱日韩一区，該凹陷風(fēng)暴沉積巖石類型豐富草国产在线视频，包括各類碎屑巖、生物灰?guī)r和火山碎屑巖粒度分布具有"高斜多跳懸式"高清无码性爱视频在线观看、多段式和"高斜一段式"等多種樣式沉積構(gòu)造發(fā)育渠模亚洲色图熟熟、沖刷面、截切等底層面侵蝕構(gòu)造和遞變層理一级做a爰片久久毛片A片高潮、塊狀層理欧美熟妇性爱A片在线A片视频、丘狀層理、洼狀層理丝袜日韩无码激情视频、平行層理等構(gòu)造亚韩色欧另类欧美在线影院，還發(fā)育有波痕和各種同生變形構(gòu)造最新男女一级性爱视频在线、生物逃逸構(gòu)造等粒度分布和沉積構(gòu)造反映出研究區(qū)兼有重力流和牽引流的水動力機(jī)制日韩网友自拍区在线观看视频网站大全。

There are three features in the minibasins induced by gravitational sliding on the slope: the firstly, feature is surface of unconformity developed by onlap on minibasin margins or surface of unconformity truncated by mass transport-complex are sequence boundary in the study area; the secondly , accommodation of gravity flow is controlled by up lift rate and sedimentation rate , and styles of filling in the minibasins are dominated by the interrelationship between the two factors; and the third , there are two stacking patterns that consists of upward of turbidite fan-hemipelagic drape mud or mass-transport complexes-turbidite fan-hemipelagic drape mud.

認(rèn)為在深水陸坡重力滑動作用所形成的微盆地內(nèi)，層序邊界表現(xiàn)為微盆地邊緣上超不整合面或重力流對下伏地層的侵蝕不整合；逆沖構(gòu)造隆升速率與沉積速率共同控制了重力流可容空間和沉積充填樣式手机看A片小视频；沉積垂向演化以塊狀搬運復(fù)合體一濁積扇－深海披覆泥或濁積扇－深海披覆泥為特征日韩一级AV不卡毛片完整版。

The allochthonous deposition mainly includes the gravity current settled sediments and the tractive current settled sediments. The autochthonous mainly includes the argillaceous deposit.

深水異地沉積主要包括重力流沉積和深水牽引流沉積兩大類；深水原地沉積主要包括深水泥頁巖沉積亚洲无码天堂在线。

Deep-water carbonate sediments include allochthonous carbonate sediments released from shallow water by gravity flow and carbonate contourite arid static autochthonous deep sea carbonate sediments.

深水碳酸鹽沈積包括深水重力流作用形成的異地沈積和非重力流沈積国产精品网站在线，在非重力流沈積中又有深水牽引流（等深流、內(nèi)波亚洲欧美日韩国产综合、內(nèi)潮汐等）沈積和靜態(tài)原地碳酸鹽沈積日韩一级片91插。

After studying the sequence stratigraphy and the provenance system, they definite the sedimentary type, sequence position, depositional area and formation mechanism of the gravity flows and set up the depositional models of the delta slump turbidite fan, slop-moving turbidity fan, nearshore subaqueous fans, sublacustrine fan and slope fan.

通過層序地層研究及物源供給系統(tǒng)分析，明確了重力流的沉積類型18岁禁止入内网站、層序位置日韩福利在线视频免费观看网址、發(fā)育部位和形成機(jī)制，建立了三角洲滑塌濁積扇人人操人人人人摸人人干、坡移濁積扇国产VA在线视频观看、近岸水下扇、湖底扇和斜坡扇共五種類型的重力流發(fā)育模式亚洲第一色日韩。

The main lithologic characteristic is that the rock types are dominated by light-colored clastic rocks reflecting the oxidation environment with a low maturity. The grain size distribution and sedimentary structure show that the rocks have the sedimentary characters of both gravity currents and tractional currents. Plant fragments are lacking and bioturbation structures are abundant and cyclic. Sandbodies are distributed in a ring shape.

其主要巖性特征為：巖石類型以反映氧化環(huán)境的淺色碎屑巖類為主国产久精品，成熟度較低，粒度分布和沉積構(gòu)造反映其兼有重力流和牽引流的沉積特點人人操人人操人人操人人操人人人操，植物碎屑貧乏而生物擾動構(gòu)造豐富且具周期性少妇无码大屁股视频XXXX，砂體呈環(huán)帶狀分布。

Dahuofang water diversion project is a typical case of this kind of engineering. This project is divided into two parts from Anshan pressure station: the up-gravity-force water diversion with double-pipe, and the down-pressure-flow part, which provides water for seven water supply station of six cities, lots of brunches, and full of ups and downs, covering many kinds of boundary conditions of modern engineering.

大伙房輸水工程就是其中一個較為典型的工程實例亚洲天堂在线视频www，該工程以鞍山加壓站為分界點將整個系統(tǒng)分為兩部分XXXXHD免费视频，鞍山上游為重力流輸水并且有一段為雙管運行，鞍山下游為壓力流天堂毛片网，一共給6個城市7個凈水廠供水欧美日韩亚洲图片，多分支，多起伏四川美女大白屁股黄毛片观看，幾乎包含了當(dāng)今輸水工程中存在的各類邊界情況看一级毛片一区二区三区免费。

After analyzing the difference of sedimentary elements, they sum up that sedimentary gravity flows are the couping result of provenance system, slop type and lake level fluctuation and that the evolution and dominant structural framework of the Liaodong lift control the sedimentary character and distribution characteristics of the gravity flows.

通過沉積要素比較分析，提出了上述重力流的發(fā)育是物源系統(tǒng)黄色网站在伦看、坡折類型和湖平面變化耦合作用的結(jié)果性饥渴艳妇k8经典A片，遼東凸起的形成演化及以其為主導(dǎo)的構(gòu)造格局決定著重力流的發(fā)育特征及分布規(guī)律。

The turbidite deposits are of both gravity flow and traction flow, forming not only fan-shaped lobes and dendritic channels, but also high tortuous channel systems by its inner circulation flow.

濁流具有重力流和牽引流的雙重屬性无码免费专区，不僅形成了扇狀的朵葉和分枝狀的水道體系爱搞入口，還通過其內(nèi)部環(huán)流形成高彎度的水道體系。