Results 31 to 40 of about 155 (140)
20 years of speleothem paleoluminescence records of environmental changes: an overview [PDF]
International Journal of Speleology, 2004 This paper discusses advance of the research on Speleothem paleoluminescence Records of Environmental Changes after it have been first introduced by the author 20 years ago.It is demonstrated that most of the progress in this field was made in result of ...
Shopov Yavor Y.
doaj
Shale Tectonics in the Hyperextended Continental Margin of the Niger Delta
Tectonics, Volume 44, Issue 7, July 2025.Abstract Based on the interpretation of a large seismic data set, we provide a comprehensive description of the structures affecting the entire Niger Delta, from the onshore domain to the deep‐offshore. The shale‐dominated delta lies on a divergent segment of the west African passive margin.
V. Spina +3 more
wiley +1 more source
Natural environments of period of the formation of Dubno paleosoil in Halych-Dniester region
Visnyk of the Lviv University. Series Geography, 2011 In the article have been suggested the analysis of main lithology-petrography characteristics of Dubno paleosoil complex in Halych-Dniester region. The natural environments of period of the formation of paleosoil have been reconstructed, based on mollusc fauna analysis.
A. Bogucki, R. Dmytruk, I. Dumas
openaire +2 more sources
Basin Research, Volume 37, Issue 3, May/June 2025.Storing CO2 in volcanic rocks has lately shown promising results; however, volcanic provinces are highly heterogeneous, implying challenges in mapping and exploring for potential CO2 reservoirs. This study showcases the importance of integrating a variety of data types across all scales in a case study in the Faroe Islands Basalt Group, North Atlantic ...
Rakul Maria Ingunardóttir Johannesen +5 more
wiley +1 more source
Permafrost and Periglacial Processes, Volume 36, Issue 1, Page 63-82, January/March 2025.ABSTRACT Arctic permafrost coasts, affected by rising sea levels and increasing coastal erosion in a warming climate, undergo significant changes. Simulating how permafrost is impacted by inundation with fresh, brackish and marine water enhances our understanding of permafrost carbon stock responses to increasingly marine conditions.
Maren Jenrich +10 more
wiley +1 more source
Palygorskite in caves and karsts: a review
Acta Carsologica, 2018 Palygorskite is fibrous mineral representing the transitional phase between chain silicates and layer silicates with modulated phyllosilicate structure.
Pavel Bosák, Nadja Zupan Hajna
doaj +1 more source
Secondary carbonates in loess-paleosoil sequences: a general review
Open Geosciences, 2011 Abstract The literature dealing with secondary carbonates in loess-paleosoil sequences is in many cases ambiguous, which means that different concepts are used for the same features, whereas certain concepts referring to different types are used as collective nouns.
openaire +2 more sources
Journal of Geophysical Research: Earth Surface, Volume 129, Issue 12, December 2024.Abstract Recovering the patterns of glacial erosion over time is key to understanding feedbacks between climate and tectonic processes. Glacial erosion rates have been shown to systematically increase worldwide toward the present since the late Cenozoic, a behavior interpreted as the response of glaciers to a cooling and increasingly variable climate ...
A. Fedotova, M. B. Magnani
wiley +1 more source
Paleosoil algoflora of pleistocene loess-soil series of Ob plateau
Environmental Dynamics and Global Climate Change, 2016 Исследование почвенных водорослей и влияния на них различных экологических факторов - одно из актуальных направлений в современной альгологии. В ходе альгологических исследований в палеопочве обнаружено 13 видов водорослей, которые относятся к 3 отделам, 4 порядкам, 4 классам, 6 семействам и 10 родам.
openaire +1 more source
Earth Surface Processes and Landforms, Volume 49, Issue 11, Page 3261-3282, 15 September 2024.Sandy loess deposits in the Fläming ridge (Brandenburg, Germany) were analysed with respect to their composition, depositional age and distribution in the landscape. They most likely originate in the lowlands to the north and were deposited during the late MIS 2 (19–14 ka), in analogy to loess deposits found further west and south.
Fabian Kirsten +7 more
wiley +1 more source