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pro vyhledávání: '"Janwari, Shazia"'
Here, we propose a novel method for representation of general spin systems using Restricted Boltzmann Machine with Softmax Regression (SRBM) that follows the probability distribution of the training data. SRBM training is performed using stochastic r
Externí odkaz:
http://arxiv.org/abs/2109.10651
Publikováno v:
In Materials & Design December 2023 236
Publikováno v:
In Applied Catalysis B: Environment and Energy 5 June 2021 286
Autor:
Rashid, Janwari Shazia AB
The Madurai Block is the largest granulite block in Southern Granulite Terrain which lies between Palghat-Cauvary shear zone in the North and Achankovil shear zone in the South. This terrain underwent extreme crustal metamorphism under ultrahigh-temp
Externí odkaz:
http://hdl.handle.net/2005/3038
http://etd.ncsi.iisc.ernet.in/abstracts/3902/G26876-Abs.pdf
http://etd.ncsi.iisc.ernet.in/abstracts/3902/G26876-Abs.pdf
Autor:
Jean, Amandine, Beauvais, Anicet, Chardon, Dominique, Bonnet, Nicolas, Jayananda, Mudlappa, Janwari, Shazia, Mathe, P.-E.
Publikováno v:
EGU General Assembly
EGU General Assembly, Apr 2017, Vienne, Austria
EGU General Assembly, Apr 2017, Vienne, Austria
International audience; Cenozoic topographic rejuvenation of divergent continental margins and their cratonic hinterland is a matter ofdebate. For instance, continental scale tilt has been advocated as a cause of Late Cenozoic relief growth of theInd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a63dc03e40d3df67c6c4f404073abe2
Autor:
Jean, Amandine, Mathe, P.-E., Beauvais, Anicet, Chardon, Dominique, Demory, François, Janwari, Shazia
Publikováno v:
European Geosciences Union, EGU General Assembly 2017
European Geosciences Union, EGU General Assembly 2017, Apr 2018, Vienne, Austria
European Geosciences Union, EGU General Assembly 2017, Apr 2018, Vienne, Austria
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fb80f5a96e5993c617cc0f21f986d2ed
Akademický článek
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