Barozh 12: Formation processes of a late Middle Paleolithic open-air site in western Armenia

P Glauberman, B Gasparyan, J Sherriff… - Quaternary Science …, 2020 - Elsevier
Abstract Barozh 12 is a Middle Paleolithic (MP) open-air site located near the Mt Arteni
volcanic complex at the margins of the Ararat Depression, an intermontane basin that …

A simple recipe for red bole formation in continental flood basalt provinces: weathering of flow-top and flow-bottom breccias

RA Duraiswami, H Sheth, P Gadpallu, N Youbi… - Arabian Journal of …, 2020 - Springer
Continental flood basalt (CFB) provinces such as the Deccan Traps show numerous inter-
flow horizons called boles, most commonly red or brown. These have been variably …

Giant plagioclase basalts: Continental flood basalt–induced remobilization of anorthositic mushes in a deep crustal sill complex

H Sheth - Bulletin, 2016 - pubs.geoscienceworld.org
Giant plagioclase basalts, rich in plagioclase megacrysts commonly 5 cm long, form
widespread lava flows and dikes in the Deccan Traps continental flood basalt province …

The Deccan tholeiite lavas and dykes of Ghatkopar–Powai area, Mumbai, Panvel flexure zone: Geochemistry, stratigraphic status, and tectonic significance

HC Sheth, GF Zellmer, EI Demonterova… - Journal of Asian Earth …, 2014 - Elsevier
Mumbai City, situated on the western Indian coast, is well known for exposures of late-stage
Deccan pillow basalts and spilites, pyroclastic rocks, rhyolite lavas, and trachyte intrusions …

Mineral magnetic and diffuse reflectance spectroscopy characteristics of the Deccan volcanic bole beds: Implications to genesis and transformations of iron oxides

P Srivastava, SJ Sangode, J Torrent - Geoderma, 2015 - Elsevier
Deccan volcanic bole beds are important indicators of paleoenvironmental conditions during
Cretaceous–Tertiary volcanism. However, little attention has been paid to iron oxide …

Mineralogy and geochemistry of various colored boles from the Deccan volcanic province: implications for paleoweathering and paleoenvironmental conditions

P Srivastava, NS Siddaiah, SJ Sangode, DC Meshram - Catena, 2018 - Elsevier
Boles are markers of hiatus in successive eruptions of the Deccan flood volcanism (DFV)
emplaced at the Cretaceous-Paleogene boundary that are interpreted to retain …

[HTML][HTML] Flood basalt hosted palaeosols: Potential palaeoclimatic indicators of global climate change

MRG Sayyed - Geoscience Frontiers, 2014 - Elsevier
Since continental sediments (in addition to the marine geological record) offer important
means of deciphering environmental changes, the sediments hosted by the successive …

Environmental magnetic properties of lateritic soils from Southwestern India

K Amrutha, AK Warrier, K Sandeep, A Jyothinath… - Eurasian Soil …, 2021 - Springer
Soil formation is influenced mainly by lithology, climate, organic matter, vegetation,
topography, and time. Soil-forming processes have been well studied in temperate regions …

Authigenic Green Mica in Interflow Horizons within Late Cretaceous Deccan Volcanic Province, India and Its Genetic Implications

P Singh, S Banerjee, K Pande, S Bhattacharya… - Minerals, 2022 - mdpi.com
Green authigenic mica, ie, celadonite, is commonly associated with submarine alteration of
basic igneous rock. However, very few studies have reported the formation of celadonite …

Early Eocene paleosol developed from basalt in southeastern Australia: implications for paleoclimate

Y Zhou, GJ Retallack, C Huang - Arabian Journal of Geosciences, 2015 - Springer
Abstract The Early Eocene Climate Optimum (EECO, 51–53 Ma) is one of several short-term
greenhouse spikes punctuating long-term Cenozoic paleoclimatic cooling. This study …