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[HTML][HTML] Compositional controls on the Lower Cretaceous Rodby Shale pore structure and surface area: A planned CCS top seal caprock for the Acorn storage site
NA AlNajdi, RH Worden, JEP Utley - International Journal of Greenhouse …, 2024 - Elsevier
Fine-grained lithologies above CCS reservoirs cannot automatically be assumed to be
mineralogically stable, or high quality top-seals to highly pressured CO 2 as saline aquifer …
mineralogically stable, or high quality top-seals to highly pressured CO 2 as saline aquifer …
[HTML][HTML] Ichnological characterization of deep-sea muddy deposits: Macrobenthic communities revealing palaeoenvironmental conditions within turbidite systems
JF Cabrera-Ortiz, J Dorador… - Palaeogeography …, 2023 - Elsevier
Traditionally, studies on turbiditic systems were mostly focused on sedimentological
features, but later some other features as bioturbation have been included. Ichnological …
features, but later some other features as bioturbation have been included. Ichnological …
[PDF][PDF] Variation of Biogenic Opal Production on the Conrad Rise in the Indian Sector of the Southern Ocean since the Last Glacial Period
JY Yang, I Minoru, H Choi, BK Khim - Ocean and Polar Research, 2023 - e-opr.org
Biological pump processes generated by diatom production in the surface water of the
Southern Ocean play an important role in exchanging CO 2 gas between the atmosphere …
Southern Ocean play an important role in exchanging CO 2 gas between the atmosphere …
[PDF][PDF] 남극해 인도양 해역에 위치한 콘래드 해령 지역의 마지막 빙하기 이후 생물기원 오팔 생산의 변화
양주연， 최혁， 김부근 - Ocean and Polar Research, 2023 - e-opr.org
Biological pump processes generated by diatom production in the surface water of the
Southern Ocean play an important role in exchanging CO2 gas between the atmosphere …
Southern Ocean play an important role in exchanging CO2 gas between the atmosphere …
新津油田, 金津層一ノ沢セクションにおける重力流堆積物の露頭スケールの岩相多様性と貯留層不均一性
栗田裕司， 辻隆司 - 石油技術協会誌, 2023 - jstage.jst.go.jp
抄録 This study exhibits a detailed lithologic description of the outcrops along the 79.95 m-
thick Ichino-sawa section of the Late Miocene-Early Pliocene Kanatsu Formation, the main …
thick Ichino-sawa section of the Late Miocene-Early Pliocene Kanatsu Formation, the main …