201981st EAGE Conference and Exhibition 2019Requires access

Reservoir Heterogeneity and Quality of Wajh Formation: Outcrop Analog Study, Red Sea Region, Saudi Arabia

Osman Abdullatif, Mutasim Osman

Open publisher page 0 citations

Abstract

Summary The early Miocene Wajh Formation represents an early rifting event alluvial fan deposits that triggered by early rifting phase in Midyan area, Red Sea region. Stratigraphically equivalent formations occur throughout the Red Sea region and the Wajh Formation represents important reservoir target in the Midyan Region, NW part of Saudi Arabia. The work is based on outcrop analog study aimed to characterize facies and depositional environment and to establish a facies depositional model. The facies are dominated by sandstones and conglomerates while the mudstones and shale represents minor percentages. On outcrop the Wajh Formation shows an overall stacked progradational succession that controlled by tectonics and sediment supply. The stratigraphic architecture and heterogeneity is influenced by shale and mudstone depositional barriers that affected sandstone vertical continuity and connectivity. However, laterally, the sandstone bodies showed good connectivity which interrupted locally by vertical faulting and fracturing at outcrop scale. At meso-scale and micro-scales reservoir heterogeneity and characteristics are affected by both depositional texture, composition and post depositional diagenetic changes. The outcrop analog study of Wajh Formation might provide guides to understand and predict controls and reservoir properties of equivalent lithofacies in the subsurface.

About this research paper

What this paper is about

Summary The early Miocene Wajh Formation represents an early rifting event alluvial fan deposits that triggered by early rifting phase in Midyan area, Red Sea region. Stratigraphically equivalent formations occur throughout the Red Sea region and the Wajh Formation represents important reservoir target in the Midyan Region, NW part of Saudi Arabia. The work is based on outcrop analog study aimed to characterize facies and depositional environment and to establish a facies depositional model. The facies are dominated by sandstones and conglomerates while the mudstones and shale represents minor percentages. On outcrop the Wajh Formation shows an overall stacked progradational succession that controlled by tectonics and sediment supply. The stratigraphic architecture and heterogeneity is influenced by shale and mudstone depositional barriers that affected sandstone vertical continuity and connectivity. However, laterally, the sandstone bodies showed good connectivity which interrupted locally by vertical faulting and fracturing at outcrop scale. At meso-scale and micro-scales reservoir heterogeneity and characteristics are affected by both depositional texture, composition and post depositional diagenetic changes. The outcrop analog study of Wajh Formation might provide guides to understand and predict controls and reservoir properties of equivalent lithofacies in the subsurface.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Summary The early Miocene Wajh Formation represents an early rifting event alluvial fan deposits that triggered by early rifting phase in Midyan area, Red Sea region. Stratigraphically equivalent formations occur throughout the Red Sea region and the Wajh Formation represents important reservoir target in the Midyan Region, NW part of Saudi Arabia. The work is based on outcrop analog study aimed to characterize facies and depositional environment and to establish a facies depositional model. The facies are dominated by sandstones and conglomerates while the mudstones and shale represents minor percentages. On outcrop the Wajh Formation shows an overall stacked progradational succession that controlled by tectonics and sediment supply. The stratigraphic architecture and heterogeneity is influenced by shale and mudstone depositional barriers that affected sandstone vertical continuity and connectivity. However, laterally, the sandstone bodies showed good connectivity which interrupted locally by vertical faulting and fracturing at outcrop scale. At meso-scale and micro-scales reservoir heterogeneity and characteristics are affected by both depositional texture, composition and post depositional diagenetic changes. The outcrop analog study of Wajh Formation might provide guides to understand and predict controls and reservoir properties of equivalent lithofacies in the subsurface.

Key concepts: Sedimentary depositional environment, Outcrop, Geology, Facies, Diagenesis, Paleontology, Rift, Tectonics

Related papers

Back to paper searchBrowse research topicsOriginal source
Reservoir Heterogeneity and Quality of Wajh Formation: Outcrop Analog Study, Red Sea Region, Saudi Arabia — Research Paper | ScholarLens