莺歌海盆地泥底辟构造成因机制的模拟实验（二）

MODEL EXPERIMENTS ON THE MECHANISM OF MUD DIAPIR STRUCTURE IN YINGGEHAI BASIN, SOUTH CHINA SEA

莺歌海盆地泥底辟构造是在热动力、重力和离心力作用下形成和演化的。介绍泥底辟成因机制的最新模拟实验结果。依据实验结果，提出了莺歌海盆地泥底辟形成和演化的热动力模式、离心力模式和重力模式。

Mud diapirs of Yinggehai Basin, South China Sea have been formed and evolved by thermody-namic, centrifugal forces, and gravity effects. This paper shows new modelling experimental photographs of mud diapir mechanism. Base on experimental results, this paper gives thermodynamic, centrifugal forces, and gravity modells in the process of formation and evolution of mud diapirs in Yinggehai Basin.