The Eocene Kohat Formation is well exposed in the Karaat hills. At this locality the lower part is composed of light brown to khaki color shale. The limestone is contained in the upper and middle part of the Formation. The ...

The early Permian sedimentary sequence of Salt Range belongs to glacio-fluvial origin of late Paleozoic Ice-age, that marks a complete transition from Ice-age period to greenhouse period. Present research work is aimed to ...

In Katha section of Central Salt Range and Pindori Oil field, Sakesar Limestone of Eocene age has been investigated for the reservoir characterization, microfacies analysis and diagenetic fabric. The research work was ...

Meyal field is located near Pindi Gheb (District Attock), 110 km southwest of Islamabad, which is bounded by latitudes 33°11'-33°22' N and longitudes 71°59'- 72° 18' E and is a part of Meyal blocks which lies in the central ...

Major objective of this research was to characterize reservoir potential and to exploit the channel reservoirs of Lower Goru Sands. These channel sands always put a challenge in front of geoscientists to exploit the channeled ...

Miano gas field is located in Middle Indus basin Pakistan, Which is the major hydrocarbon producing fields of the area. Main purpose of the research is reservoir characterization and seismic inversion to find the reservoir ...

Tree rings have been used in various applications to reconstruct past climates as well as to assess the effects of climatic and environmental change on tree growth. The study focused on growth of Pinus roxburghii (Chir ...

Water is very vital for domestic and agricultural use. Pakistan is an agricultural country. Pakistan has two large reservoirs i.e. Mangla and Tarbela dams whose capacity is decreasing due to sedimentation. Pakistan needs ...

Miano gas field located in Central Indus Basin, Pakistan, is chosen to perform seismic interpretation of deeper horizons of Cretaceous age reservoir. Before performing interpretation, data loading, its navigation, quality ...

Indus basin is usually subdivided into sub-basins by the help of regional positive features called paleo-highs In the Middle Indus Basin, these highs provide some magnificent stratigraphic entrapment geometry especially ...