Abstract The Scourie dyke swarm in the Lewisian foreland of northwest Scotland provides key constraints on the Paleoproterozoic evolution of the North Atlantic craton. High‐precision U‐Pb geochronology identifies two distinct intrusive phases at ∼2.41–2.38 Ga and ∼2.00 Ga.
M. Mirzaei +4 more
wiley +1 more source
Quantitative Characterization of Micropore Structure and Seepage Characteristics of Diagenetic Facies and Their Implications for Development in the Highly Inhomogeneous Chang 9 Reservoir, Ordos Basin. [PDF]
Gu X +6 more
europepmc +1 more source
Abstract Offshore freshened groundwater (OFG) is a significant yet underexplored component of global water resources, occurring widely along many continental margins. However, its dynamics remain poorly constrained due to limited offshore observations and the absence of robust evaluation models for unambiguous emplacement interpretation.
Chong Sheng +5 more
wiley +1 more source
Source-to-sink coupling and spatiotemporal evolution during multiphase rifting: The Jurassic-Cretaceous Lishu fault depression, Southeastern Songliao Basin. [PDF]
Wang K, Zhou Y, Yan J, Zhang Y.
europepmc +1 more source
Abstract Integrating multiple detrital mineral systems provides a powerful framework for reconstructing source‐region tectonothermal evolution because different minerals record complementary aspects of magmatic and metamorphic processes. Glacial diamictites are particularly valuable for this approach because extensive glacial erosion can sample broad ...
Lijun Wang +7 more
wiley +1 more source
Nitrogen Isotopic Composition of Crude Oils from the Dongpu Depression, Bohai Bay Basin, Eastern China: Implications for Sedimentary Redox Conditions and Oil-Source Correlation. [PDF]
Chen J +6 more
europepmc +1 more source
Abstract The soles of ophiolites preserve slices of oceanic crust metamorphosed to amphibolite‐ to granulite‐facies conditions beneath heavily deformed mantle peridotites, providing key records of fluid and mass transfer across nascent subduction interfaces.
Louise Mérit +11 more
wiley +1 more source
Development of Organic Pores in the Gufeng and Longmaxi Formation Shale, Sichuan Basin: Combined Effects of Bioprecursor, Pore Filling, and Mineral-Organic Interactions. [PDF]
Wang Z, Hu G, Pang Q.
europepmc +1 more source
Abstract Whether the Songduo metamorphic belt represents an in situ Paleo‐Tethyan suture within the Lhasa Terrane or far‐traveled allochthonous high‐pressure slices, and how Permian mantle activity along the North Gondwana margin relates to subsequent Tethyan evolution, remain central questions in Tibetan tectonics.
Yuan‐Bo Ma +9 more
wiley +1 more source
Quantitative reconstruction and sedimentary response of a Jurassic paleodrainage system. [PDF]
Li N +7 more
europepmc +1 more source

