Zobrazeno 1 - 10
of 140
pro vyhledávání: '"Matteo Alvaro"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-5 (2024)
Abstract Natural processes such as earthquakes, volcanism and orogenesis are controlled by plate tectonics which, in turn, depend on how rocks and minerals, the building blocks of Solid Earth, deform under different environmental conditions. The rheo
Externí odkaz:
https://doaj.org/article/af0b999207e943209cd1f4cb23040a96
Publikováno v:
Communications Chemistry, Vol 7, Iss 1, Pp 1-5 (2024)
Extraterrestrial carbon gives insights into the origin of life and processes that took place billions of years ago in our solar system. Here, the authors provide an overview of what is known and of unanswered questions with a meteoritical focus.
Externí odkaz:
https://doaj.org/article/8681ffa392be4d2ab092c261d4792b31
Autor:
Michele Vezzola, Solveig Tosi, Enrico Doria, Mattia Bonazzi, Matteo Alvaro, Alessio Sanfilippo
Publikováno v:
Journal of Fungi, Vol 9, Iss 10, p 976 (2023)
The aim of this study was to evaluate the potential of Aspergillus tubingensis in extracting metals from rocks simulating Martian regolith through biomining. The results indicated that the fungal strain produced organic acids, particularly oxalic aci
Externí odkaz:
https://doaj.org/article/423645e37f3c49d9a64d862c172cbebd
Publikováno v:
Communications Chemistry, Vol 5, Iss 1, Pp 1-3 (2022)
Most of our knowledge about the chemical composition of the Earth’s interior is primarily retrieved by indirect observations, experiments and calculations that are limited to simple compositions. Here, the authors present the investigation of inclu
Externí odkaz:
https://doaj.org/article/203479f3d0c545438dda3105b3f4374e
Publikováno v:
Annual Review of Earth and Planetary Sciences. 51:331-366
Upon exhumation and cooling, contrasting compressibilities and thermal expansivities induce differential strains (volume mismatches) between a host crystal and its inclusions. These strains can be quantified in situ using Raman spectroscopy or X-ray
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d68634658f2edc77260f9592b1159e1
https://doi.org/10.1146/annurev-earth-031621-112720
https://doi.org/10.1146/annurev-earth-031621-112720
Publikováno v:
Geology. 51:23-27
Elastic thermobarometry of host-inclusion systems for back-calculating pressure (P) and temperature (T) conditions of inclusion entrapment relies on the assumption that the hostinclusion rheology is purely elastic. In this study, we have explored bot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5221fa94101285e311ef20a9ca496ac9
https://doi.org/10.1130/g50431.1
https://doi.org/10.1130/g50431.1
Autor:
Tingting Gu, Martha G. Pamato, Davide Novella, Matteo Alvaro, John Fournelle, Frank E. Brenker, Wuyi Wang, Fabrizio Nestola
Publikováno v:
Nature Geoscience. 15:950-954
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2fd9033e63cc2f27cb0cd1bcbb9035d7
https://doi.org/10.1038/s41561-022-01024-y
https://doi.org/10.1038/s41561-022-01024-y
Autor:
Rick Verberne, Hugo W. van Schrojenstein Lantman, Steven M. Reddy, Matteo Alvaro, David Wallis, Denis Fougerouse, Antonio Langone, David W. Saxey, William D. A. Rickard
Publikováno v:
Journal of Metamorphic Geology. 41:3-24
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6e60b436cc2ae9177ec4c02cf165d76
https://doi.org/10.1111/jmg.12686
https://doi.org/10.1111/jmg.12686
Earthquakes are generated through the brittle failure of rocks at depth. While earthquakes are generally caused by far–field tectonic stresses, the atomic–scale mechanisms that actually trigger brittle failure in dry ductile crustal rocks are sti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91aa290d7670daa6ec115e1b5bbf5631
https://doi.org/10.5194/egusphere-egu23-13491
https://doi.org/10.5194/egusphere-egu23-13491
Autor:
Sofia Lorenzon, Davide Novella, Paolo Nimis, Steven D. Jacobsen, Emilie Thomassot, Martha G. Pamato, Loredana Prosperi, Alessandra Lorenzetti, Matteo Alvaro, Frank Brenker, Franco Salvadego, Fabrizio Nestola
Publikováno v:
Geology. 50:996-1000
Natural diamonds and their inclusions provide unique glimpses of mantle processes from as deep as ~800 km and dating back to 3.5 G.y. Once formed, diamonds are commonly interpreted to travel upward, either slowly within mantle upwellings or rapidly w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78594499bed4146b7dbc3dd193415d2c
https://doi.org/10.1130/g50111.1
https://doi.org/10.1130/g50111.1