This chapter analyzes and discusses the formation conditions, distribution characteristics, and induced engineering hazards of the representative special geological bodies, namely mud diapirs, mud volcanoes, coral reefs, and ancient river channels.
Therefore, integrated analysis is required for the determination of deep hydrocarbon sources, including geological (altitude, log response, color, and mud content) and geochemical (biomarker, carbon isotope) analysis.
For geological disasters such as landslides and mud slides, it is possible to assign damage state based on whether the building structure has been damaged, the position relative to the geological disaster area, and the degree of burial.
The accuracy of the soil analytical method was examined by the standard reference material MAG-1 (marine mud from the United States Geological Survey).
Seismologists study geologic events and geological time.
However, enhancing weak diffraction events related to the body of mud volcano guarantee defining the geological structure in post stack imaging.
The present study aims to investigate disaster preparedness and perception of abrupt geological disasters (such as rock avalanches, landslide, mud-rock flows etc) in mobility-disadvantage group living in coastal rural area of China.
In addition to these geological characteristics, it is known that the Murono mud volcano is located in a strain concentration belt (e.g. Sagiya et al. 2000).
This study aims on evaluating the onboard data and subsequent geological interpretations by conducting shorebased analyses of drilling mud gas samples.
Mud volcanoes not only increase complexity of the geological condition, but also reduce the S/N ratio of the data due to strong absorption coefficient of mud.
