底辟构造的英文

• diapir structure
• diapiric structure
• diapirstructure

• "底"英文翻译    bottom; base
• "辟"英文翻译    monarch; sovereign; ruler
• "构造"英文翻译    structure; construction; con ...
• "地幔底辟构造" 英文翻译 :    mantle diapir; mantlediapir
• "页岩底辟构造" 英文翻译 :    shale diapire
• "不完全底辟构造" 英文翻译 :    immature diapirs
• "底辟盐丘构造" 英文翻译 :    diapir salt structure
• "底辟盐体构造" 英文翻译 :    diapir salt structure
• "底辟重褶构造" 英文翻译 :    diataphral tectonics
• "底辟" 英文翻译 :    diapire; diapiric fold; piercement dome
• "生长底辟；生长刺穿构造" 英文翻译 :    growth diapir
• "次底辟" 英文翻译 :    sub-diapir
• "底辟核" 英文翻译 :    diapir core; diapircore
• "底辟体" 英文翻译 :    diapris
• "底辟岩" 英文翻译 :    diapirite
• "底辟背斜" 英文翻译 :    diapiric anticline
• "底辟花岗岩" 英文翻译 :    diapiric granite
• "底辟母岩层" 英文翻译 :    diapiric mother bed
• "底辟侵入" 英文翻译 :    diapir penteration; diapiric intrusion
• "底辟上升" 英文翻译 :    diapiric rise; diapiric suprise; diapiric uprise
• "底辟体核部" 英文翻译 :    diapir core; diapiric core
• "底辟物质" 英文翻译 :    diapiric material
• "底辟作用" 英文翻译 :    diapirism; tiphon
• "底辟穹丘" 英文翻译 :    diapir dome
• "底辟褶皱" 英文翻译 :    diapiric fold

• Furthermore , the depositing model of gas hydrates in the structure of diapirs is construed in this paper
  笔者在进行综合分析的基础上，对底辟构造中天然气水合物的成矿模式进行了进一步的分析和探讨。
• The background for the formation of the diapirs is analyzed and the existence of gas hydrates is predicted in south china sea
  文中对南海底辟构造发育的地质背景进行了分析，并对南海天然气水合物的发育和赋存进行了预测。
• The structure of diapirs can be regarded as the result of the pressure of inner gases upthrusted from the lower strata , and the migration of gases from deeper strata
  底辟构造可能是地层内部圈闭气体由于压力释放上冲的结果，也可能是气体向上运移的通道。
• The research on the structure of diapirs in the area of gas hydrates show that there are close relationships between the form and accumulation of gas hydrates and the diapirs
  摘要世界上天然气水合物发现地区的地质构造特征研究表明，底辟构造和水合物的形成与聚集有较为密切的关系。
• In the high - resolution seismic profile , to directly identify the diapir is often difficult due to much similarity between diapir and the invasion of igneous rock , thus leading to multi - resolution
  在高分辨率地震剖面解释中，直接识别泥底辟构造存在一定困难，主要因为泥底辟构造和火成岩侵入体在形态上十分相似，容易造成解释的多解性。
• The relationships between the accumulation of gas hydrates and the typical diapirs in passive continental margin are summarized in primary in this paper which suggest that the factors in passive continental margin including the thick sediment layers , plastic substance , high pressure fluid , outboard volcanic activities and the process of stretch - rupture provide favorable conditions for the formation of the diapirs which can form advantageous environment for gas hydrates coming into being
  初步总结了被动大陆边缘中典型底辟构造与天然气水合物的成矿关系，认为被动陆缘内巨厚沉积层、塑性物质与高压流体、陆缘外侧的火山活动及张裂作用，为底辟构造发育提供了条件，形成了水合物成矿的有利空间。
• Surrounding these special problems met in gas hydrates exploration and through study of high - precision magnetic survey , the sea test by r / v haiyang 1y that is owned by guangzhou marine geological survey in dongsha area of the south china sea , systematical analysis of the test result and combination interpretation of magnetic survey with seismic profile , the authors successfully employ the method to recognize the truth or false of the diapir in seismic profile by integrating total field of high - precision marine magnetic measurement with its gradient change
  本文就目前天然气水合物调查中存在的这些特殊技术问题，通过对海上高精度磁力测量技术方法研究、广州海洋地质调查局“海洋四号”船在南海北部东沙海域的海上试验、对试验结果的系统研究分析以及磁测和地震剖面两种手段的综合解释，成功地尝试了用高精度海洋磁测成果中的磁力总场和梯度变化特徵来识别水合物勘探中高分辨率地震剖面上的泥底辟构造真伪的技术方法。