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Dykes and their magma overpressure

Dykes are essentially magma filled fractures within the earth’s crust often formed by the pressure imparted by the intruding magma. Magnitude of the magma overpressure has been traditionally determined utilizing elastic properties of the host rock and the complete dimension i.e., full length and maximum width of the fractures.
Tridib Kumar Mondal   +1 more
openaire   +1 more source

Overpressured Layer Chromatography

2003
Ernő Tyihák   +2 more
openaire   +1 more source

Mechanisms for overpressure generation in the bonan sag of Zhanhua depression, Bohai Bay Basin, China

Marine and Petroleum Geology, 2021
Sheng He, Tian Dong, Yuanjia Han
exaly  

Experimental study on explosion overpressure and flame propagation characteristics of simulated vertical dome oil tank

Journal of Loss Prevention in the Process Industries, 2022
Xinsheng Jiang, Jianjun Liang
exaly  

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