Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Anmol Naik"'
Autor:
Anmol Naik, Dhanashree Ratra, Aniruddha Banerjee, Daleena Dalan, Sourabh Jandyal, Girish Rao, Parveen Sen, Muna Bhende, V Jayaprakash, Pradeep Susvar, Jaydeep Walinjkar, Chetan Rao
Publikováno v:
Indian Journal of Ophthalmology, Vol 67, Iss 4, Pp 523-529 (2019)
Purpose: Enhanced S-cone syndrome (ESCS), a rare disorder, is often misdiagnosed as other forms of retinal degenerations, which have a poorer prognosis than ESCS. The aim of this study is to report the varied clinical features of ESCS and distinguish
Externí odkaz:
https://doaj.org/article/30b98867ceab4317bc814d2dca981200
Publikováno v:
Geological Magazine. 159:1415-1436
The primary features (morphologies, structures, textures) of volcanic lava flows are determined by parameters such as composition, temperature, crystallinity, viscosity, flow velocity, strain rate and cooling rate. However, lava flows are open system
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c361532968d67428a1b2d2228693c34c
https://doi.org/10.1017/s0016756822000279
https://doi.org/10.1017/s0016756822000279
Publikováno v:
International Journal of Earth Sciences. 111:379-399
Voluminous silicic (rhyolitic–dacitic) eruptive units overlie mafic lavas in many continental flood basalt (CFB) provinces of the world. These silicic units comprise lavas as well as pyroclastic deposits, including lava-like ignimbrites, and many w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94f8208c0b803dbf2e6fe52c3a75c48d
https://doi.org/10.1007/s00531-021-02119-4
https://doi.org/10.1007/s00531-021-02119-4
Publikováno v:
Geochemistry. :125984
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cacad662c3683884447b7eb24303ecc
https://doi.org/10.1016/j.chemer.2023.125984
https://doi.org/10.1016/j.chemer.2023.125984
Publikováno v:
Journal of Earth System Science. 130
The western Indian volcanic rifted margin, and its large-scale tectonic feature called the Panvel flexure, formed at 62.5 Ma during the late stages of Deccan Traps flood volcanism. We present a geological account of late-stage (≤ 62.5 Ma) Deccan vo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30f00e9a92145f5fa94e04275553f8d4
https://doi.org/10.1007/s12040-021-01654-7
https://doi.org/10.1007/s12040-021-01654-7
Publikováno v:
Bulletin of Volcanology. 82
The physical volcanology of widespread rhyolites and dacites overlying flood basalt lavas in the northwestern and northern parts of the 65.5-Ma Deccan Traps, India, is poorly known. We show that these are not lava flows but high-grade (welded and rhe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f667c8953999008b5a192a6916e6d64
https://doi.org/10.1007/s00445-020-01381-9
https://doi.org/10.1007/s00445-020-01381-9
Publikováno v:
Journal of Volcanology and Geothermal Research. 419:107389
In many continental flood basalt (CFB) provinces of the world, widespread silicic lavas and ignimbrites overlie the mafic lavas. Our knowledge of this post-flood basalt silicic volcanism in the Deccan Traps CFB province of India remains limited. Here
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8f33037047a4ab9f9e4be28706d8be0
https://doi.org/10.1016/j.jvolgeores.2021.107389
https://doi.org/10.1016/j.jvolgeores.2021.107389
Publikováno v:
Journal of Volcanology and Geothermal Research. 404:107024
Mount Pavagadh (840 m) in the northern Deccan Traps, India, is mainly composed of mafic lava flows (picrites, ankaramites, mugearites, basalts) and capped by rhyolites. Rhyolites also found at lower elevations, on and around the mountain, are thought
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0a8276ed5ee05254407c46f93c1d8c3
https://doi.org/10.1016/j.jvolgeores.2020.107024
https://doi.org/10.1016/j.jvolgeores.2020.107024