The Pliocene-Recent Euphrates river system: Sediment facies and architecture as an analogue for subsurface reservoirs
The Tigris-Euphrates is a continental-scale fluvial system, around 2800 km in length, which drains over 1 million km2 of SW Asia. The system originated in the Late Miocene and developed into the principal axial drainage system of the region, which follows broad regional structural features of the Me...
Main Authors: | , , , , , , |
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Format: | Article |
Language: | English |
Published: |
KeAi Communications Co., Ltd.
2020-10-01
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Series: | Energy Geoscience |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S2666759220300524 |