Lithofacies identification can provide qualitative information about rocks. It can also explain rock textures which are importantcomponents for hydrocarbon reservoir description Sarvak Formation is an important reservoir which is being studied in the Marun oilfield, in the Dezful embayment (Zagros basin). This study establishes quantitative relationships between digital well logs data androutin...

Noise cancelation is the process done to remove out-of-range anomalies and make better edge boundaries interpretation. One of most challenging issues in describing gravitational maps separating related shallow sources from deep ones. Furthermore, Existing noise can it arduous separate blurred boundaries. In this study SE Iran, surveying was carried out areas west Qeshm Hormuz islands a regular ...

Field observations, together with the results of gas chromatography–mass spectrometry (GC-MS) and stable carbon isotope analysis bitumen, coupled fluid inclusion microthermometry analyses closely associated vug- fracture-filling columnar calcite in Upper Cretaceous Bekhme Formation, Kurdistan Region Iraq, suggest that degradation crude oil was caused by regional incursion meteoric waters. This ...

[1] Large topographic belts along convergent margins have been recognized with the ability to slowdown the kinematics of subduction over geologically short time periods (i.e., few Myr), because their associated gravitational spreading provides significant resistive force within the framework of plate tectonics. The record of past and present-day plate kinematics provides important constraints o...

The Govanda Formation was deposited during the Early-Middle Miocene Epoch in intermountain areas between Zagros Suture and Imbricate zones. Paleoecology depositional environment of has been studied detail Mergasor Penjwen districts for first time. formation these two sections from bottom to top is comprised thick bedded, oyster chert bearing conglomerate, pebbly sandstone, red-brown shale silts...

In this study, four well-exposed outcrops of the Asmari Fm in the southeastern part of the Izeh Zone of the Zagros Mountains were measured and sampled. In this region, the Asmari Fm is Oligocene to Early Miocene in age as determined by large benthic foraminifera. Based on depositional geometries, biogenic contents and lateral and vertical variations of facies, three depositional models are prop...