Seismic interpretation of mobile shales is challenging, mostly because of their unclear
seismic expression. Imaging of mobile shales is difficult because of their low seismic …

The intricate convergence of tectonic plates and the interplay between landmasses and
oceans in subduction zones give rise to marine geo-hazards, encompassing catastrophic …

The complex interplay between thrust wedge deformation, tectonically-induced fluid
overpressures, and the complex phases of wedge-top sedimentary depositional systems in …

The active structures of the Iranian Makran, especially the presence of normal faults, vary
laterally in the upper plate of the subduction zone, and their relationship with the deep …

Sediments deposited into foreland basins can provide valuable insights related to the
geological evolution of their hinterlands. Located in the peripheral foreland of the South …

The Makran accretionary prism is located at the junction of the Eurasian Plate, Arabian Plate
and Indian Plate and is rich in natural gas hydrate (NGH) resources. It consists of a narrow …

Mud volcanoes are dynamic geological features releasing methane (CH 4), carbon dioxide
(CO 2), and hydrocarbons, harboring diverse methane and hydrocarbon-degrading …

Mud pools are chemically similar to volcanism and are considered a pollution risk to
ecosystems. The mud pools of Los Negritos, Michoacán, Mexico, additionally present …

Volcanic gas sampling and SO 2 flux measurements were performed on Taftan volcano
(3920 m height, SE Iran, Makran volcanic arc) and Damavand volcano (5610 m height …

A comprehensive geochemical investigation was carried out to characterise the sediment
and water seeping out from mud volcano in Kampung Meritam, Limbang, northern Borneo …