TY - JOUR AU - Budai, S AU - Willems, CJL AU - Colombera, L AU - Westaway, R TI - Influence of sedimentary architecture on static connectivity and geothermal doublet performance (Mezőberény, SE Hungary) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 164 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106820 UR - https://m2.mtmt.hu/api/publication/34806109 ID - 34806109 N1 - Export Date: 12 April 2024 Correspondence Address: Budai, S.; Dipartimento di Scienze Della Terra e Dell'Ambiente, Via Ferrata 1, Italy; email: soma.budai@unipv.it LA - English DB - MTMT ER - TY - JOUR AU - Li, Yanan AU - Xue, Jingqi AU - Wang, Shuai AU - Ye, Zhaorui AU - Yang, Jun TI - Mixed siliciclastic-carbonate-tuffaceous sedimentation in a rift lacustrine basin: A case study of the Lower Cretaceous Jiufotang Formation in the Luxi sag, Songliao basin JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 164 PY - 2024 SP - 106851 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106851 UR - https://m2.mtmt.hu/api/publication/34805262 ID - 34805262 LA - English DB - MTMT ER - TY - JOUR AU - Zhang, Y AU - Zhu, G AU - Li, X AU - Ai, Y AU - Duan, P AU - Liu, J TI - Resistance of eogenetic dolomites to geochemical resetting during diagenetic alteration: A case study of the lower Qiulitage Formation of the Late Cambrian, Tarim Basin JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 164 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106822 UR - https://m2.mtmt.hu/api/publication/34781884 ID - 34781884 LA - English DB - MTMT ER - TY - JOUR AU - Ping, H AU - Deng, W AU - Chen, H AU - Guo, Y AU - Kong, K AU - Yang, X AU - Liu, J TI - Fluid inclusion calibration of clumped-isotope solid-state reordering in dolomite: Implication for thermal history reconstruction in deeply buried reservoirs JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 163 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106773 UR - https://m2.mtmt.hu/api/publication/34781781 ID - 34781781 LA - English DB - MTMT ER - TY - JOUR AU - Liu, X AU - Qiu, N AU - Feng, Q TI - The thermal history of Permian carbonate strata reconstructed with clumped isotopes and U–Pb dating: Eastern Sichuan Basin, SW China JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 163 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106767 UR - https://m2.mtmt.hu/api/publication/34781770 ID - 34781770 LA - English DB - MTMT ER - TY - JOUR AU - Cao, Hong AU - Sun, Zhilei AU - Zhang, Xilin AU - Zhang, Xia AU - Wu, Nengyou AU - Geng, Wei AU - Jiang, Zike AU - Bin, Zhai AU - Yunbao, Sun AU - Jiang, Xuejun AU - Zhang, Dong AU - Dong, Aiguo TI - Formation of dolomites from the newly discovered ancient cold seep in the Middle Dongsha area of the South China Sea JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106829 UR - https://m2.mtmt.hu/api/publication/34779517 ID - 34779517 LA - English DB - MTMT ER - TY - JOUR AU - Pang, Jungang AU - Colombera, Luca AU - Mountney, Nigel P. AU - Guo, Ji'an AU - Yang, Kewen AU - Li, Wenhou TI - Mapping palaeoshorelines of river-dominated deltas in lacustrine ramp settings: Application of sedimentological analyses to the Triassic Yanchang Formation (Ordos Basin, China) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 164 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106797 UR - https://m2.mtmt.hu/api/publication/34760468 ID - 34760468 LA - English DB - MTMT ER - TY - JOUR AU - Kairouani, H. AU - Abbassi, A. AU - Zaghloul, M.N. AU - El, Mourabet M. AU - Micheletti, F. AU - Fornelli, A. AU - Mongelli, G. AU - Critelli, S. TI - The Jurassic climate change in the northwest Gondwana (External Rif, Morocco): Evidence from geochemistry and implication for paleoclimate evolution JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 163 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106762 UR - https://m2.mtmt.hu/api/publication/34750320 ID - 34750320 N1 - Laboratory Research and Development in Applied Geosciences (LRDGA), Earth Science Department, FST-Tangier, University Abdelmalek Essaadi, Tetouan, Morocco Dipartimento di Scienze, Università Degli Studi Roma Tre, Rome, Italy LR3G laboratory, Earth Science Department, FS-Tetouan, University Abdelmalek Essaadi, Tetouan, Morocco Dipartimento di Scienze Della Terra e Geoambientali, Università Degli Studi di Bari Aldo Moro Bari, Italy Dipartimento di Scienze, Universita Della Basilicata, Potenza, 85100, Italy Dipartimento di Ingegneria Dell'Ambiente, Università Della Calabria, CS, Rende, 87036, Italy Export Date: 21 March 2024 Correspondence Address: Kairouani, H.; Laboratory Research and Development in Applied Geosciences (LRDGA), Morocco; email: kairouanihajar@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - El-Yamani, Mahmoud Samir AU - John, Cédric M. AU - Bell, Rebecca TI - Mechanism of island dolostones formation in the Cretaceous calcitic ocean: Insights from the Mid-Pacific Guyots JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 163 PY - 2024 SP - 106741 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106741 UR - https://m2.mtmt.hu/api/publication/34715355 ID - 34715355 AB - Dolomite is common in carbonate successions. There is an ongoing debate about the origin of ancient massive dolostones. Recent studies suggest widespread syndepositional and early-burial dolomitisation by normal and near-normal seawater, in the rock record, than previously recognised. Seawater dolomitisation is ubiquitous in Cenozoic islands but Cretaceous counterparts are rare, except for Resolution and Allison guyots, Mid-Pacific Mountains. We explored their dolomitisation conditions and the implications on our understanding of Cretaceous normal seawater syndepositional and near-surface dolomitisation. Integrating geochemical and borehole data reveals temporal overlap between 87Sr/86Sr ages of dolomites, and K/Ar and 40Ar/39Ar ages of the basement. Dolomites near basaltic basement exhibit 42-times Fe-enrichment compared to normal seawater dolomites. Host-rock thermal modelling suggested that δ18Odol temperatures are ∼18–29 °C higher than concurrent temperatures. Seismic interpretation and seismic facies forward modelling demonstrate a spatial overlap between dolomites and magmatic sills in both guyots. Accordingly, magmatically driven hydrothermal dolomitisation is proposed, which promoted dolomitisation by providing high heat flow, increasing seawater circulation, and overcoming limited dolomitisation potential of Cretaceous seawater. The H2O–CO2–SO2–HCl-rich magmatic-hydrothermal acidic fluids would mix with seawater causing slight modification by leaching Mg and Fe from basaltic basement. Consequently, magmatically active Cretaceous islands had greater potential for seawater dolomitisation than counterparts with ceased magmatism, due to increased heat flux and slight increase in Mg:Ca of dolomitising fluids. Our findings imply that deep-seated island dolostones don't only form by deep cold seawater below calcite saturation depth. Instead, magmatism appears crucial in this study and potentially other locations (e.g. Xisha Islands). The absence of dolostones in other Cretaceous islands supports previous models of reduced effectiveness of massive dolomitisation by Cretaceous normal seawater, questioning interpretations of syndepositional and near-surface dolomitisation. Thus, caution is advised when interpreting these dolomites by considering additional factors (dolomite geometry, geological settings, and dolomitisation age), as they may share characteristics with syndepositional and near-surface normal seawater dolomites. LA - English DB - MTMT ER - TY - JOUR AU - Zheng, B AU - Zhou, R AU - Mou, C AU - Ge, X AU - Hou, Q AU - Zhao, J AU - Howard, D TI - Origins of the Upper Permian reef-dolostone and reservoir evolution in northern South China JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 162 PY - 2024 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2024.106748 UR - https://m2.mtmt.hu/api/publication/34689478 ID - 34689478 LA - English DB - MTMT ER -