diapir 中文意思是什麼
diapir
解釋
刺穿構造-
For the exploration of gas hydrates, it is of great significance to study such geological structures as mud diapir and mud volcano
摘要在天然氣水合物勘探中，海底的泥底辟和泥火山構造是重要的研究對象。 -
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
本文就目前天然氣水合物調查中存在的這些特殊技術問題，通過對海上高精度磁力測量技術方法研究、廣州海洋地質調查局「海洋四號」船在南海北部東沙海域的海上試驗、對試驗結果的系統研究分析以及磁測和地震剖面兩種手段的綜合解釋，成功地嘗試了用高精度海洋磁測成果中的磁力總場和梯度變化特徵來識別水合物勘探中高解析度地震剖面上的泥底辟構造真偽的技術方法。 -
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
在高解析度地震剖面解釋中，直接識別泥底辟構造存在一定困難，主要因為泥底辟構造和火成巖侵入體在形態上十分相似，容易造成解釋的多解性。 -
A study on the formation mechanism of diapir in kunyang group, central yunnan
滇中昆陽群刺穿構造形成機制研究 -
There are 3 types of reservoir for the continuing subsidence type basin, there are diapir reservoir, fault reservior, drape reservoir, and the source rock is apart from the reservoir, they are contact by fault ; and there are anticline reservoir, fault reservoir, incline reserve ir, mudstone reservoir under the denudation area, and the source rock is contact with the reservoir
以沉降為主要趨勢的盆地的油氣藏有底辟構造油氣藏、斷層油氣藏、披覆構造油氣藏，其烴源巖與油藏在空間上是分離的，並通過斷層相連；剝蝕區以下的油氣藏有背斜油氣藏或斷層油氣藏、向斜油氣藏及泥質巖油氣藏，其烴源巖和油氣藏可有密切的接觸關系。 -
The distribution and accumulation of coa are controlled by mud - diapir development
平面上具有分區分塊性，縱向上co2分佈具有分帶分層性。 -
When diapir fractures opened, entering of hot fluid into reservoirs may cause dissolution of carbonate minerals, and when diapir fractures closed, carbonate minerals precipitated in high temperature condition
底辟斷裂開啟時，深部富c02熱流體進入儲層，導致碳酸鹽礦物溶解；通道閉合時，高溫使碳酸鹽礦物沉澱。
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