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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。Both shallow and deep gas plays are present in the mud diapir belt.

盆地广泛发育断裂、底辟构造,影响着水合物的分布。Faults and diapir develop widely and influence the distribution of gas hydrate.

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岩盐造成的蘑菇状或柱塞状的刺穿构造。一般有上覆盖岩。A mushroom-shaped or plug-shaped diapir made of salt, commonly having an overlying cap rock.

底辟物质由盐岩为主的塑性层组成。Diapir was mainly composed of some salts, and minor soft mudstone or other plaster sediments.

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。Mud diapir is an important geologic phenomenon related to gas accumulation in Yinggehai Basin.

刺穿构造是指老构造岩片刺穿于新地层中的构造形迹。Diapir structure is a special structural feature with the old tectonic massif pierced in the new formation.

在某些地质时期还与幔源岩浆的底垫对地壳或岩石圈的改造有关。Some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.

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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。There are extraordinary active thermal fluids in the mud diapir zone of central depression in Yinggehai basin.

在第四纪时期,该地区上地幔仍然继续其底辟上涌过程。All these results have shown that an upper mantle diapir had continued to occur during the Quaternary in this area.

并在综合分析国内外流力破裂研究成果的基础上,论述了流体底辟形成的机制和地质背景。Besides, the mechanism and geologic setting of fluid diapir are analyzed, on the basis of the theory of fluid fracturing.

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

因此,泥底辟构造带无疑是莺—琼大气区最有勘探开发前景的领域之一。Therefore the mud diapir structure belt is one of the most potential areas for exploration and development in Ying Qiong giant gas area undoubtedly.

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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岩中。The deposit is evidently controlled by diapir and structure, and ore bodys are located in cataclastic dolomite of Lüzhijiang Formation Fengshan member.

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

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。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 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.

高分辨率黄河三角洲典型的地震地层和解释地层剖面、浅地层剖面和钻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。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.

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