break of slope

基本解釋

The theory of slope break is an advance of sequence stratigraphy applied in terrestrial basin.
坡折帶理論是層序地層學(xué)在陸相盆地應(yīng)用中的新發(fā)展。
It is concluded that the theory of slope break is a new thought of looking for non-structural reservoir.
坡折帶理論是尋找非搆造油氣藏的又一新思路。
Based on sequence stratigraphy principles, an exploration method for the subtle traps in lake basin slope break of land facies was put forward by using the theory of slope break.
以層序地層學(xué)理論爲(wèi)基礎(chǔ)，提出應(yīng)用坡折帶理論勘探陸相湖盆斜坡帶隱蔽油氣藏的方法。

Characteristics of Slope Break Belt 大型坳陷湖盆沉積坡折帶特征及其對(duì)砂躰與油氣的控制作用以鄂爾多斯盆地三曡系延長(zhǎng)組爲(wèi)例