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Data for: Eccentricity control on fluvial sedimentation in the tropics during the Middle-Late Pennsylvanian icehouse (~306–314 Ma, Upper Silesian Basin)

NIAID Data Ecosystem2026-05-02 收录

天文旋回地层学

古气候沉积学

数据链接：

https://data.mendeley.com/datasets/6mtgshd3r6 数据链接链接失效反馈

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资源简介：

Dataset S1: Lithofacies ranks, boreholes PoZ IG-1, MB-B, Che IG-1, G-2 AW, G-5 Dąb and G-13 Dąb; Upper Silesian Basin

应用场景：

创建时间：

2025-03-10

沉积地质

天文旋回地层学

This high-resolution total gamma (API) dataset from the Fort Ancient and Clarksville members of the Waynesville Formation (Late Ordovician, Katian) shows a shift from obliquity and precession dominanc

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Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1)@en

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冰川动力学

Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean

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Table3_Climate-Controlled Coastal Deposition of the Early Permian Liangshan Formation in Western South China.xlsx

古气候沉积学

二叠纪冰川消融响应

During the late Paleozoic ice age, tropical coastal depositions have been widely linked to high-frequency sea-level variations, but their linkage with the associated climate change was not fully under

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Long-Term Fine-Grained Sediment Records in a Drainage System in Arid China: A New Perspective from Paleo-Climatological Records and Simulations

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Atmospheric particulate matter (PM 2.5 and PM 10) can adversely affect human health and also has impacts on climate and precipitation. Much research has been done on the transport of human-made fine-g

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Eccentricity Control on Fluvial Sedimentation in the Tropics During the Middle-Late Pennsylvanian Icehouse (~306-314 Ma, Upper Silesian Basin)

天文旋回地层学

古河流沉积动力学

This study examines the Cracow Sandstone Series (CS), which provides a snapshot of the Middle to Late Pennsylvanian (~306-314 Ma) fluvial sedimentation in the eastern equatorial Pangea (Upper Silesian

DataCite Commons2025-03-11 更新30

Data for: Eccentricity control on fluvial sedimentation in the tropics during the Middle-Late Pennsylvanian icehouse (~306–314 Ma, Upper Silesian Basin)

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