Titlebook: Recent Research on Sedimentology, Stratigraphy, Paleontology, Geochemistry, Volcanology, Tectonics, ; Proceedings of the 2 Attila Çiner,Ste

athlete’s-foot

Early to Middle Cambrian Fluvial-Aeolian Interplay and Marine Transgression Depositional System of tdded sandstone. The member fills relatively low topographic depression on the underlying Huqf Supergroup surface and lacks marine signatures reflecting deposition in an isolated inland freshwater lake. The middle member comprises intervals of cobble conglomerates grading upward into pebbly to granul

BIBLE

Lithofacies Associations and Depositional System of the Muti Formation, Oman Mountainscribed to identify the lithofacies associations and depositional setting of the formation. These lithofacies are correlated across various sections to help understand their distribution and depositional environments. The Muti Formation thickness ranges from 13.4 to 179 m and comprises nine lithofaci

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strain

Late Cambrian-Early Ordovician Hybrid-Energy Deltaic System of the Peri-Gondwana Terranes: An Examplarge-scale reactivation surfaces, sigmoidal cross-bedding, climbing ripples, and flaser bedding indicate tidal flats and delta distributary channels of the lower delta plains. Wave and storm facies, including wave ripples and small-scale hummocky cross-stratification, represent a mouth bar/shoreface

Arthr-

Genesis of Grain-Coating Clays and Their Effect on the Development of Feldspar Overgrowths: A Case S shows honeycomb-like texture and cornflake textures with filamentous terminations. The chlorite forms ~ 3 μm thick envelop rimming, seemingly the entire detrital grains and at grain-to-grain contacts. The chlorite also shows a honeycomb-like texture and curved platelet morphologies. The described i

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货物

Depositional Facies and Sea-Level Variation of the Cryogenian Glacial System: An Example from the Oud section and consist of thick massive mud-prone, clast-poor dilute diamictite intervals. They are of rainout ice-rafted based diamictites, sourced by iceberg-based debris flows, and deposited towards the distal area of the basin, distant from an active ice margin. Local glacier features (i.e., ice-

cortex

吞噬

The Aptian Incised Valleys Recorded in the Maestrat Basin (E Iberia)en the truncated sedimentary successions and the incised valley fills. Therefore, these drops in relative sea level are interpreted to be mainly of eustatic origin. The late early and early late Aptian sea-level drops occurred respectively in < 0.9 and < 3 Myr according to the current version of the

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