Orbital forcing and paleoenvironmental changes across the upper Ordovician glaciation-lower Silurian hot shale in the Risha gas field, northeast Jordan-Reference-Cited by-同舟云学术

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Orbital forcing and paleoenvironmental changes across the upper Ordovician glaciation-lower Silurian hot shale in the Risha gas field, northeast Jordan

Published:2024-10 Issue: Volume:168 Page:107040
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Farouk Sherif,Abdeldaim Ahmed,Qteishat Abdelrahman,Ahmad Fayez,Mohammed Ibrahim,Al-Kahtany Khaled,Powell John H.

Funder

King Saud University

Co-creation place formation support program

Publisher

Elsevier BV

Reference73 articles.

1. Ground water origin and movement in the upper Yarmouk Basin, Northern Jordan;Abu-Jaber;Environ. Geol.,2008

2. The lower silurian (hot shale) source rocks of western Iraq: depositional model and stratigraphic distribution;Al-Hadidy;The Iraqi Geological Journal,2023

3. Tectono-stratigraphic framework and evolution of the northwestern Arabian Plate, Central Jordan;Al-Hseinat;Tectonophysics,2023

4. Determination of clay minerals using gamma ray spectroscopy for the Zubair Formation in Southern Iraq;Al-Jafar;J. Pet. Explor. Prod. Technol.,2022

5. Accurate petrophysical interpretation of carbonate using the elemental capture spectroscopy;Alameedy;ECS) Iraqi Journal of Chemical and Petroleum Engineering,2023

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