Titlebook: Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a; Proceedings of the 1 Attila Çiner,San

完成才能战胜

Post-oligocene Tectono-Eustatic Fluctuations and Their Influence on the Stratigraphy of Eastern Arabthe low-lying region between the Al-Hajar Mountains and the coast of the Gulf of Oman. The group is divisible into three tectonostratigraphic successions represented by three formations: Sultan Qaboos University (SQU), Suwadi, and Barzaman, in ascending order. The SQU Formation consists of conglomer

用不完

gruelling

Establishment of Geological Age Under the Constraints of Astronomical Cycles in Dongying Saggeological age has always been a scientific problem. Astronomical cycle analysis is an effective method developed for high-resolution stratigraphic research in recent years. We apply this method to improve the accuracy of the stratigraphic age of the ash-deficient section of lacustrine fine-grained

Deduct

vocation

一起

Spectral Gamma-Ray Variability Within Carbonate Lithofacies: An Example from the Early Triassic Lowery facies. Spectral gamma-ray is widely used in depositional facies and sequence stratigraphic analysis. Here, spectral gamma-ray U, Th, and K measurements from two logged sections of the Early Triassic Lower Mahil Formation (Upper Khuff-equivalent, KS1) of Al Jabal Al-Akhdar (Saiq Plateau and Wadi

为敌

defendant

单调女

Early Pliocene Benthic Foraminifera of the Southeastern Coast of Cap Bon Peninsula (Northern Tunisia of the Jrêba section (Nabeul region, southeastern coast of the Cap Peninsula, Tunisia). A diversified micro-faunistic content was documented, consisting of 36 species of benthic foraminiferal belonging to 26 genera and 21 families. Among these species: ., . ., ., C., . These species are ecologicall

全神贯注于

The Geochemistry of Biotite from TTG Batholiths and A-type Complexes (Silet Region, Hoggar, Algeria)) batholiths and four A-type complexes. All of them are exposed in the central part of the Silet terrane (western Hoggar, Algeria) and crosscut Pharusian volcano-sedimentary series. According to Nd isotope values, the rocks are geographically arranged in two narrow N-S oriented bands separated by th