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

方面

書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a影響因子(影響力)




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a影響因子(影響力)學科排名




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a網(wǎng)絡公開度




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a網(wǎng)絡公開度學科排名




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a被引頻次




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a被引頻次學科排名




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a年度引用




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a年度引用學科排名




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a讀者反饋




書目名稱Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology a讀者反饋學科排名

Foment

Upper Pleistocene-Holocene Coastal Depositional Sediments of the Farwah Spit, NW Libyarganic matter (TOC up to 3.05%), deposited within a lagoon, and protected from the sea by Holocene sand spits. Locally, close to the eastern inlet, the lagoonal facies pass into rippled sands, interpreted to record flood delta deposits. Landward, the cycle is represented by supratidal sand and mudst

率直

培養(yǎng)

Paleoecology, Paleoenvironment, and Petroleum Potential of middle-upper Cretaceous Calabar Flank Sedbris were recognized in this study. They comprise phytoclasts (degraded and structured), opaque, amorphous organic matter (AOM) and palynomorphs. These palynofacies suggested highly proximal shelf or basin and marginal dysoxic-anoxic basin paleoenvironments of deposition. In addition, Kerogen type I

繼承人

Post-oligocene Tectono-Eustatic Fluctuations and Their Influence on the Stratigraphy of Eastern Arabi Formation is a carbonate tongue with abundant corals, calcareous algae, larger benthic foraminifera (LBF), echinoids, and mollusks. The LBF fossils indicateLanghian-Serravalian age. The underlying SQU Formation is envisaged to be early Miocene in age. The Barzaman Formation is dominated by pebble-

拋媚眼

New Time-Expanded Chronostratigraphic Column of Northern Iraq During Cretaceous and Tertiaryand their boundary is assigned as gradational in the new chronostratigraphic column. The column also includes the lateral merging of the Kolosh Formation and the lower part of the Red Bed Series with the Walash Formation (Group). The study considers these three units as deposits of a large foreland

Mawkish

Tonometry

Well Log Sequence Stratigraphic Analysis of the Upper Carboniferous-Early Permian Haushi Group in So (TST), and finally, the lowstand system tract (LST). The lower Gharif Member deposited consecutively and shared the transgressive system tract (TST) with the upper Al-Khlata Member. This system tract ended with marine shales marking a maximum flooding surface. The middle Gharif reflects a highstand

nonradioactive

費解