diapir中文,diapir的意思,diapir翻译及用法

2026-05-06 01:39 浏览次数 20

diapir

英['daɪəpɪə(r)]美['daɪəˌpɪr]

n. [地质] 底辟;挤入构造

diapir 英语释义

英语释义

  • a domed rock formation where a core of rock has moved upward and pierced through the more brittle overlying strata

diapir 片语

片语

diapir intrusion底辟侵入

magma diapir巖浆底辟

diapir penetration底辟刺穿作用

clay diapir粘土刺穿构造

diapir breccia因民角砾巖底辟角砾巖

diapir zone底辟带

falling diapir下降盐刺穿

growth diapir生长底辟

diapir zones底辟构造带

diapir 例句

英汉例句

  • some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.

    在某些地质时期还与幔源巖浆的底垫对地壳或巖石圈的改造有关。

  • the middle-deep beds are very important new hydrocarbon exploration area in the yinggehai basin where there are some mud diapir belts with abnormal high temperature and pressure.

    莺歌海盆地泥底辟带异常高温高压的中深层目的层是该盆地新的油气勘探领域。

  • the traps were formed by the upward arch of diapiric fluid, and episodic diapir activity determined hydrocarbon episodic migration.

    主要圈闭由底辟流体上拱形成,底辟活动的幕式发育决定了油气幕式运移。

  • on this basis, combining the distribution feature of sulfide in mantle and the model of mantle diapir uprising, the model of formation and evolution of second stage magma has been advanced.

    在此基础上,结合地幔中硫化物的分布特点和地幔巖块底辟上升模式,提出了第二侵入期巖浆的形成演化模式。

  • in the laizhouwan depression, the sha4 member of the paleogene shahejie formation attains thick salt and gypsum which have uplifted and formed salt diapir and pillow in the kl112 area.

    莱州湾凹陷沙河街组四段含有较厚的巖盐和膏盐层,并在kl112地区发生聚集隆起,形成典型的盐底辟(盐枕)构造。

  • both shallow and deep gas plays are present in the mud diapir belt.

    在天然气水合物勘探中,海底的泥底辟和泥火山构造是重要的研究对象。

  • diapir was mainly composed of some salts, and minor soft mudstone or other plaster sediments.

    底辟物质由盐巖为主的塑性层组成。

  • all these results have shown that an upper mantle diapir had continued to occur during the quaternary in this area.

    在第四纪时期,该地区上地幔仍然继续其底辟上涌过程。

  • aiming at exploring the medium-deep layers of mud diapir belt in the yinggehai basin, cnooc drilled two wells at the end of 20th century.

    针对莺歌海盆地底辟带中深层,中国海洋石油总公司在2 0世纪末批準并上鉆了两口探井。

  • there are extraordinary active thermal fluids in the mud diapir zone of central depression in yinggehai basin.

    莺歌海盆地中央坳陷泥底辟带是一个热流体非常活跃的地区。

  • mud diapir is an important geologic phenomenon related to gas accumulation in yinggehai basin.

    泥拱是莺歌海盆地的重要地质现象,它与油气聚集有密切关系。

  • the thrust faults, folds, strike-slip faults and magmatic diapir structures were formed in the lower layer;

    下构造层发育逆沖断层、褶皱、走滑构造和巖浆底辟构造;

  • the evolution of mud-fluid diapir in yinggehai basin is the result of regional stress field variation and (over-pressure) system formation and evolution.

    莺歌海盆地的泥-流体底辟构造发育演化是区域构造应力场变化和超压体系形成演化的结果。

  • as the main and typical structure in diapir area, df1-1 diapir develops a lot of faults and cracks, virtually related with gas accumulation.

    根据df1-1的成藏特点 ,强调断裂系统与天然气运聚的相互促进关系 ,建立了断裂系统与天然气成藏关系模式 。

  • the interpretation of a typical sub-bottom profile reveals that the diapir of the yellow river delta resulted from the interior deformation of soft prodelta layers at the delta front.

    高分辨率黄河三角洲典型的地震地层和解释地层剖面、浅地层剖面和鉆孔资料联合解释表明,海底刺穿的发源层来自于河口沙坝下部的前三角洲相软弱层变形。

  • a mushroom-shaped or plug-shaped diapir made of salt, commonly having an overlying cap rock.

    巖盐造成的蘑菇状或柱塞状的刺穿构造。一般有上覆盖巖。

  • diapir structure is a special structural feature with the old tectonic massif pierced in the new formation.

    刺穿构造是指老构造巖片刺穿于新地层中的构造形迹。

  • the central shale diapir zone is distributed with numerous diapir-anticlines and nose structures which are adjacent to hydrocarbon sources , being most prospective.

    中央泥底辟构造带分布众多的泥拱背斜及鼻状构造并邻近油气源,是最有利的构造带。

  • the oil and gas reservoirs with distinctive features were widely formed in the mud diapir structure belt because of the special geological conditions in yinggehai basin.

    莺歌海盆地特有的地质特征使泥底辟构造带广泛形成具有特色的油气藏。

  • faults and diapir develop widely and influence the distribution of gas hydrate.

    盆地广泛发育断裂、底辟构造,影响着水合物的分布。

  • the deposit is evidently controlled by diapir and structure, and ore bodys are located in cataclastic dolomite of lüzhijiang formation fengshan member.

    矿床明显受刺穿体和构造的控制,矿体赋存于绿汁江组凤山段白云巖中。

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