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英語人>網(wǎng)絡(luò)例句>basin 相關(guān)的網(wǎng)絡(luò)例句
basin相關(guān)的網(wǎng)絡(luò)例句

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與 basin 相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò)www色色色色色色com,僅供參考]

But, as China's Yellow River basin population and the increasing economic and social development, the development and use of the Yellow River reached unprecedented levels, the obvious contradiction between the Yellow River basin interprovincial water, the Yellow River flow frequency accelerated.

但是国产强奸中文字幕系列精品片,隨著我國黃河流域人口的不斷增加和經(jīng)濟(jì)社會的發(fā)展免费黄色性爱网站,對黃河的開發(fā)利用達(dá)到前所未有的程度黄片一A毛片,黃河流域跨省區(qū)用水矛盾突出久久久噜噜噜久久三级,黃河斷流頻率加快黄色的视频国产在线观看。

According to the tectonic evolution,structure of section,sequence relationship and source-reservoir-cap composition of foreland basins,the foreland basins can be divided into two types including epicontinental foreland basin and intracontinental foreland basin.

依據(jù)前陸盆地的發(fā)展演化午夜麻豆国产精品视频、剖面結(jié)構(gòu)、層序關(guān)系和生儲蓋組合特點(diǎn),將前陸盆地劃分為陸緣前陸盆地和陸內(nèi)前陸盆地兩大類亚州一二区,其中陸緣前陸盆地包括周緣前陸盆地和弧后前陸盆地国产在线视频超彭。

The Ordos basin is a large Mesozoic intracontinental basin superimposed on the Paleozoic North China craton which contains abundant oil and gas resource.

鄂爾多斯為一個(gè)我國陸上第二大沉積盆地,是大型克拉通疊合盆地国产精品女主播国产区,油氣資源豐富女人的奶头(无遮挡)免费。

It is shown that, in some areas, such as Tarim Basin, Beishan and Qaidam Basin, although the results derived from traditional Airy model and lithospheric isostasy model are close, the lithospheric isostasy model can explain the nature of the mass balance in a more reasonable way.

計(jì)算結(jié)果表明,在一些地區(qū)2021国产高清视频,如塔里木盆地亚洲福利一区二区三区美女导航、北山和柴達(dá)木盆地,盡管巖石圈均衡模型和Airy模型得到了一致的海拔值日本人人操人人爱,但巖石圈均衡模型更能體現(xiàn)均衡過程的物理本質(zhì)AA级毛片视频免费观看;除青藏高原造山帶外的多數(shù)塊體,巖石圈均衡模型的計(jì)算結(jié)果更接近觀測海拔和地表垂直運(yùn)動狀態(tài)又黄又爽的欧美视频;總體上狼友视频免费看,考慮地幔巖石圈熱結(jié)構(gòu)影響后,中國大陸各地區(qū)的均衡結(jié)果普遍優(yōu)于傳統(tǒng)的均衡模型色婷婷国产精品视频一区二区。

The slope belts of rifted lacustrine basin in Bohai Bay Basin are very important for hydrocarbon accumulation.

渤海灣盆地?cái)嘞莺璧男逼聨怯蜌饩奂闹匾獔鏊?/p>

The slope belt s of rifted lacustrine basin in Bohai Bay Basin are very important for hydrocarbon accumulation.

渤海灣盆地?cái)嘞莺璧男逼聨怯蜌饩奂闹匾獔鏊?/p>

Late Triassic Ordos Basin is one of the largest oil-bearing lacustrine basin.

橫跨陜甘寧的晚三疊世鄂爾多斯盆地是一個(gè)富含油氣的大型內(nèi)陸沉積盆地天美传媒无码。

From macro to micro and from qualitative to quantitative evaluation, this paper, applicating the theory and technological method of sequence stratigraphy、seismic stratigraphy婷婷色色综合区、 reservoir sedimentology, combining with multispecialty and mutisubject theory that used geology, log, seismic, mathematics and earth physics and basing on synthetic application of regional geology, core, log, seismic and petrophysical property data, has studied the inner structure and characteristic of sequence国产产一区二区三区久久毛片国语、system tract and depositional system. Combining with high resolution seismic data and log data, this paper makes a profound analysis of the space pattern and reservoir predictability of depositional system on oil and gas pools of honghaoersute sag.

中文題名陸相斷陷湖盆層序地層特征與油氣勘探副題名以二連盆地洪浩爾舒特凹陷下白堊統(tǒng)為例外文題名 Terrigenous sequence stratigraphy characteristic hydrocarbon exploration of fault-depressed lacustrine basin:a case study of early cretaceous,Honghaoersute sag女性毛片A,Erlian basin 論文作者譚榮導(dǎo)師趙霞飛教授杜金虎教授級高級工程師學(xué)科專業(yè)礦產(chǎn)普查與勘探研究領(lǐng)域\研究方向陸相層序地層學(xué)與區(qū)域油氣評價(jià)學(xué)位級別博士學(xué)位授予單位成都理工大學(xué)學(xué)位授予日期2002 論文頁碼總數(shù)128頁關(guān)鍵詞層序地層油氣勘探二連盆地洪浩爾舒特凹陷油氣藏館藏號BSLW /2002 /P618.13 /325 本文采取從宏觀到微觀成年人黄色视频网站,從定性到定量的研究思路国免费自拍视频,應(yīng)用層序地層學(xué)白白色在线免费观看、地震地層學(xué)、儲層沉積學(xué)的理論和技術(shù)方法欧洲一级人与嘼视频免费播放,結(jié)合區(qū)域地質(zhì)91精品国产色综合久久久久、巖芯、測井三级黄韩国性爱、地震800av..com、物性資料,采用多專業(yè)亚洲熟女福利、多學(xué)科理論和方法相結(jié)合国产精品国产自线拍免费下载。

Silicalites, predominated by pelitic silicalite, occur in collisional zones and back-arc basins. In the collisional zones, they occur as rock sheet as an important part ofophiolitic mé lange, belonging to ophiolitic mélange type silicalite. In the back-arc or interarc basin, they occur as pelitic silicalite intercalation varying in thickness, characteristic of "silica merl",and belonging to abyssal back-arc basin type or carbonate type silicalite. In the magmatic arc, they occur as intercalation related to volcanic hydrotherm or volcalic exhalation, belonging to volcanic arc type silicalite.

在硅質(zhì)巖方面:岡底斯構(gòu)造帶侏羅系硅質(zhì)巖主要屬泥質(zhì)硅質(zhì)巖,在各個(gè)碰撞結(jié)合帶和弧后盆地中均有產(chǎn)出永久性爱视频一区二区,主要的產(chǎn)出狀態(tài)有:①在碰撞結(jié)合帶中呈巖塊產(chǎn)出www無码视频,構(gòu)成蛇綠混雜巖的重要組成部分,屬蛇綠混雜巖型硅質(zhì)巖;②在弧后或弧間盆地中呈厚度不等的泥質(zhì)硅質(zhì)巖夾層產(chǎn)出欧洲激情无码专区,常具"硅灰泥"特征亚洲原创中文字幕区,屬弧后深水盆地型硅質(zhì)巖;③呈夾層狀產(chǎn)于弧火山巖系中人人干人人操123,屬火山熱液或火山噴氣型硅質(zhì)巖六月婷婷一区。

In recent years, a few researchers have been assured that the Mesozoic Ordos basin is a foreland basin.

近年來,有不少研究者將其中生代構(gòu)造屬性劃歸"前陸盆地"东北老熟妇爱456视频。

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And Pharaoh spoke to Joseph, saying, Your father and your brothers have come to you.

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