斷陷盆地 的英文怎麼說
中文拼音 [duànxiànpénde]
斷陷盆地
英文
downfaulted basin-
Lying in the east of heilongjiang province, yishu graben is a cenozoic fault basin comprising two large second - class structural units, i. e., tangyuan and fangzheng fault basins
摘要依舒地塹位於黑龍江省東部，為新生代斷陷盆地，湯原斷陷和方正斷陷為其兩個面積較大的二級構造單元。Compared with lehua manganese deposit in pingxiang - leping faulted basin, which is a sedimentary hydrothermal superimposed type, both orebodies are different obviously in orebody scale, ore type and tenor of manganese etc., it should be a deposit with different genetic type
並與萍一樂斷陷盆地內的沉積加熱液疊改型樂華錳礦床進行了對比分析，二者在礦體規模、礦石類型、錳品位等方面存在顯著差別，應屬不同成因類型的礦床。Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )
通過研究有以下成果及認識：鄂爾多斯盆地及其周緣地區沉積蓋層可劃分為五大構造層序，盆地的形成和演化分為六大構造階段：太古代至古元古代基底形成階段、中新元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?早古生代華北陸表海盆演化階段、晚古生代?早中生代華北克拉通坳陷演化階段、中生代中晚期大鄂爾多斯內陸盆地演化階段及獨立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。Guided by the theory of sequence stratigraphy and petroleum system using cores, lithologic log or well - logging, biostratigraphic and seismic data, adopting seismic inversion constrained to well data, digital analysis technology, basin modeling, test method and so on, and adopting an integrated study technology, aiming at lower exploration in chagan depression, this work put forward a new research thoughtfulness, technic flow and method system that is an integrated study by " looked upon sequence stratigraphy as a base, looked upon petroleum system as a integer, combing with each other closely " and tie in qualitative analysis and quantitative analysis and applied synthetically new theory, new technology and new method
以層序地層理論和含油氣系統思想為指導，利用巖心、鉆/測井、古生物以及地震資料，採用井約束下的地震資料反演技術、計算機技術、盆地模擬技術和各種分析實驗手段等綜合分析方法，針對查干凹陷勘探程度低的特點，提出了斷陷盆地「以層序地層分析為基礎、含油氣系統為整體（系統）和二者緊密結合」以及定性與定量相結合，綜合應用新理論、新技術和新方法的研究思路、技術路線和方法體系。One of the most important discoveries in this study is the regional exhalative sedimentary mineralization along the bobai - chenxi faulted zone in early palaeozoic, based on which, the metallogenic model of diplogenesis is developed for the fozichong orefield
博白-岑溪斷裂帶在早古生代為一同生斷裂系統，在拉張環境下沿斷裂帶形成了一地塹型斷陷盆地。Santanghu basin is a congruent & reconstruct innertief, which developed on the basis of rift - fault basin of permian
三塘湖盆地是一個在二疊紀裂谷-斷陷盆地基礎上發展起來的疊合、改造型山間盆地。Hegang coal field, of the type of a ( inland ) faulted basin far from the sea, was formed in the early neo - jurassic age about 140 million years ago
鶴崗煤田約形成於一億四千多萬年前的晚侏羅世初期，是遠海內陸斷陷盆地型煤田。The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin, and shangrao and mingxi basins are the continental margin fault basins in the early triassic
早三疊世的中下揚子混積盆地屬克拉通邊緣盆地，而上饒和明溪碎屑巖盆地則為大陸邊緣斷陷盆地。In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric, karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
目前開展的可有效利用的地下水資源調查評價將該區劃分為隆起帶裸露巖溶分佈區、沉降帶邊緣褶皺構造控制巖溶分佈區和斷陷盆地隱伏巖溶分佈區。According to granite ages cutting ruptures, mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin, deformation age are limited, that are 100 ~ 65ma for one and form 65ma to the present for two and three
根據斷裂截切的花崗巖體年齡、同期褶皺變形的含礦石英脈年齡以及斷裂兩側斷陷盆地的形成時代，大致限定第1期變形時代為100 65ma ，第2 、 3期變形時代為65ma現今。After have systematically studied sequence stratigraphy of chagan depression, a analysis method of high precision sequence stratigraphic framework in fault - depressed lacustrine basin. the core of the establishing framework is exploration - significant identify of sequence, division of 2, 3, 4, 5 grades sequence and analysis of base - level based on lithologic log or well - logging, high - resolution seismic inversion constrained to well data. then using the results of 2d seismic data, and interpret sequence to enhance the precision of interpretation
斷陷盆地高精度層序地層格架建立的核心是用鉆/測井和井約束條件下的高解析度儲層橫向預測剖面等高解析度資料進行具有勘探意義的二、三、四和五級層序的界面識別、層序劃分和基準面變化分析，在此基礎上標定常規地震剖面，進行區域層序地層分析，達到提高層序地層解釋精度的目的。With an area of 5300 km2, dongpu depression is located in the southwest of lin - qing depression, bohaiwan basin, bounded with lu - xi uplift by lan - liao fault in the east, with nei - huang uplift by chang - yuan fault in the west, with lan - kao heave by the north feng - qiu fault in the south, with xin country depression by ma - ling fault in the north, while spreading along nne defection, taking on the forms of being wide in the south, and narrow in the north. it is a rift fault depression basin with the characteristics of striking, with the basement being the paleozoic and mesozoic, and the capping beds being the cenozoic
東濮凹陷位於渤海灣盆地臨清坳陷西南端，東側以蘭聊斷裂為界與魯西隆起為鄰，西側以長垣斷裂為界與內黃隆起相接，南以封丘北斷層為界與與蘭考凸起相鄰，北以馬陵斷層為界與與莘縣凹陷相望，是以古?中生界為基底，以新生界為蓋層，古近紀形成的拉分走滑?裂谷型箕狀斷陷盆地。Through studying the stratigraphic framework of tectonic sequence, the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes
晚白堊世至古近紀區域構造背景發生重大變化，構造層序記錄了晚燕山期地殼快速均衡隆升，伸展斷陷盆地形成演化過程。In this paper, the main conclusion have been put forword as following : 1 yinachang fe - cu - ree deposit occurred in wuding - lufeng volcanic fault deporssion during the initial stage of kunyang rift
主要認識如下： 1 、迤納廠礦床產于昆陽裂谷初期形成的祿豐-武定火山斷陷盆地中。Sequence types and subtle reservoirs exploration in continental rift - subsidence basin
陸相斷陷盆地層序類型及隱蔽圈閉預測Genetic features of western geothermal resources in tai - lai downfaulted basin
泰萊斷陷盆地西部地熱資源的成因Discussion on the formation and origin of the shiguai mesozoic rift basin in inner mongolia
內蒙古石拐中生代斷陷盆地形成與成因初探Preliminary study on the minerogenetic model of mesozoic volcanic - magmatic rocks in eastern jilin, china
雲南斷陷盆地淺循環巖溶水賦存規律初步研究In liaohe rifted basin, du66 block is situated on the middle part in the western slope in the western depression, and is a typical thin - interbedded reservoir with heavy oil
摘要杜66塊位於遼河斷陷盆地西部凹陷西斜坡中段，為一典型的薄互層狀普通稠油油藏。Mound form, ice erosion rock basin and broken to fall into basin spread all over at plateau, china most heavy zh zh body traces, namely " daocheng ancient to ice cap ". .
丘狀冰蝕巖盆和斷陷盆地遍佈於高原上，是中國最大的古冰體遺跡，即"稻城古冰帽" 。 。 。分享友人