Results 1 to 10 of about 6,571,111 (245)
Reconstructing Chemical Weathering Intensity in the Mekong River Basin Since the Last Glacial Maximum [PDF]
AbstractHigh‐resolution clay mineralogy and major element geochemistry of Core SO18383‐3 collected off the Mekong River mouth in the southern South China Sea have been investigated, aiming to reconstruct sediment provenance and chemical weathering intensity since the last glaciation.
Thanakorn Jiwarungrueangkul +2 more
exaly +2 more sources
Abstract Chemical weathering of continental silicates is a crucial geological process in regulating Earth’s long-term climate and participating in global carbon cycle. The increasing aridity and active tectonic settings in the northeastern Tibetan Plateau since the middle Miocene, combining the global cooling background, make this region ideal for ...
Xing Jian, Hanjing Fu, Xiaotian Shen
exaly +2 more sources
The hydrochemical characteristics of watersheds are influenced by many factors, with chemical weathering and human activities exerting the most substantial influence. Performing a quantitative evaluation of the factors contributing to the chemical weathering of rocks is of significant scientific importance. This research zeroes in on the Qingtang River
Fang Guo, Fan Liu
exaly +2 more sources
Intensive Chemical Weathering in the Arctic During the Miocene Climatic Optimum [PDF]
The Arctic today has shallow, chemically immature, and frost-dominated weathering regimes. At Sokli, Finland (68°N), a 70 m deep palaeo-weathering profile is developed in a Devonian carbonatite pipe that represents fundamentally different past weathering environments.
Hall, Adrian M.; id_orcid 0000-0001-9985-8944 +5 more
openaire +1 more source
Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation [PDF]
Significance At least two extreme glaciations (dubbed as snowball Earth events), each lasting millions of years and affecting the entire globe, occurred during the Cryogenian Period (∼720–635 Ma). These glaciations are recorded by globally distributed glacial deposits overlain by cap carbonates.
Kang-Jun, Huang +7 more
openaire +2 more sources
Intense Chemical Weathering at Glacial Meltwater-Dominated Hailuogou Basin in the Southeastern Tibetan Plateau [PDF]
Climate warming has caused rapid shrinkage of glaciers in the Tibetan Plateau (TP), but the impact of glacier retreat on the chemical denudation rate remains largely unknown at the temperate glacial basins. The chemical weathering processes were examined at a temperate glacial basin (HLG) in the southeastern TP based on comprehensive data from the ...
Xiangying Li +8 more
openaire +1 more source
Relevance. Diatomites and their transitional differences formed in the Paleocene–Eocene marine basin are one of the most widespread in the near-surface occurrence of sedimentary rocks in the vast territory of the Trans-Urals. At the same time, with regard to the genetic aspects of such rocks, the discussion on the fundamental sources of silica for ...
Smirnov P.V. +3 more
openaire +1 more source
Abstract The alteration of rainfall patterns, the possible worldwide increase of mean temperatures, and the recurrence of extreme climatic events roughly describe climate change, as widely perceived. Accordingly, geochemical investigations are researching if climate change may accelerate the weathering of crustal rocks, through its net effect on the ...
openaire +2 more sources
Distinctive volcanic ash-rich lacustrine shale deposition related to chemical weathering intensity during the Late Triassic: Evidence from lithium contents and isotopes. [PDF]
Liu Q +8 more
europepmc +1 more source
The evolution of the Earth's surface iron cycle. [PDF]
Scholz F, Doetterl S, Hardisty DS.
europepmc +1 more source

