To investigate the subsurface structure surrounding Main Frontal Thrust (MFT) in central Nepal, we drilled and cored sediments to depths of 45–100 m at 10 sites. Our boreholes were located along previously acquired high-resolution seismic profiles across MFT imaging upper 1–2 km subsurface, which revealed a beveled erosional surface hanging wall above broad, gentle anticline, as well growth str...

The purpose of the article. article is devoted to study one from forms syndynamics in Late Pennsylvanian time, namely phytocoenogenesis. phytocoenogenesis ancient plant communities, i.e., formation new types palaeophytocoenoses, based on research vegetation diversity that reflected ecological-floristic classification phytocoenoses Donets Basin by Brown-Blanquet method. Material and methods. phy...

Geological evidence for extensive non-polar ice deposits of Amazonian age indicates that the current cold and dry climate of Mars has persisted for several billion years. The geological record and climate history of the Noachian, the earliest period of Mars history, is less certain, but abundant evidence for fluvial channels (valley networks) and lacustrine environments (open-basin lakes) has b...

this study is focused on the biostratigraphy, sedimentary environments, facies distribution, and sequence stratigraphy of the coniacian–santonian sediments of tange-bulfaris section. five assemblage zones have been recognized by distribution of the foraminifera in the study area. assemblage zone 1(chara ostracods zone) is coniacian in age and occurs in the lower part of the succession. assembla...