Zobrazeno 1 - 10
of 173
pro vyhledávání: '"Craig E. Manning"'
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-7 (2019)
The amount of carbon stored in closed hidden reservoirs is unknown. Here the authors use a computational approach to study the evolution of carbon species and observe polymerization of carbon atoms at high pressures, illustrating the potential for a
Externí odkaz:
https://doaj.org/article/bbc6c9c7157845a98d70bd6e717c9ae3
Publikováno v:
Elements. 16:375-380
Aqueous fluids are critical agents in the geochemical evolution of Earth’s interior. Fluid circulation and fluid–rock reactions in the Earth take place at temperatures ranging from ambient to magmatic, at pressures from ambient to extreme, and in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb2d79fee498bd4a4d3c3956444b7093
https://doi.org/10.2138/gselements.16.6.375
https://doi.org/10.2138/gselements.16.6.375
Autor:
Craig E. Manning, Maria Luce Frezzotti
Publikováno v:
Elements. 16:395-400
Fluids are essential to the physical and chemical processes in subduction zones. Two types of subduction-zone fluids can be distinguished. First, shallow fluids, which are relatively dilute and water rich and that have properties that vary between su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9c9ae0fb6614a82baef16ab8e5c9954
https://doi.org/10.2138/gselements.16.6.395
https://doi.org/10.2138/gselements.16.6.395
Publikováno v:
Geochimica et Cosmochimica Acta. 279:119-142
The interaction of fluids with rock-forming minerals plays an important role in the chemical evolution of mafic and ultramafic rocks in the lower crust and upper mantle. Recent work highlights the importance of salt-rich fluids in element transport i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c00df143003df0ebe76bfc22978fda8
https://doi.org/10.1016/j.gca.2020.03.035
https://doi.org/10.1016/j.gca.2020.03.035
Autor:
Craig E. Manning, Matteo Masotta, Veronica Stopponi, Yoshio Kono, Vincenzo Stagno, Piergiorgio Scarlato
Publikováno v:
Carbon in Earth's Interior
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a7e3e4cb8f624e101e6b5b3d35fa257f
https://doi.org/10.1002/9781119508229.ch19
https://doi.org/10.1002/9781119508229.ch19
Publikováno v:
Carbon in Earth's Interior
Understanding the interactions between calcite and aqueous solutions is important when studying the deep carbon cycle. The present study investigates the solubility of calcite in salt-H2O fluids at 700 °C and 8 kbar. The investigated salts included
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbb3db1e0f0ba48473da0e6ec28364b8
https://doi.org/10.1002/9781119508229.ch21
https://doi.org/10.1002/9781119508229.ch21
Autor:
Terry Plank, Craig E. Manning
Publikováno v:
Nature. 574:343-352
A hidden carbon cycle exists inside Earth. Every year, megatons of carbon disappear into subduction zones, affecting atmospheric carbon dioxide and oxygen over Earth's history. Here we discuss the processes that move carbon towards subduction zones a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d48f00b3eaa2c717f83dd33fb32d2917
https://doi.org/10.1038/s41586-019-1643-z
https://doi.org/10.1038/s41586-019-1643-z
Publikováno v:
Nature. 569:542-545
Amorphous water ice comes in at least three distinct structural forms, all lacking long-range crystalline order. High-density amorphous ice (HDA) was first produced by compressing ice I to 11 kilobar at temperatures below 130 kelvin, and the process
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2848e17d87178c5d6cf6680189ba9b4
https://doi.org/10.1038/s41586-019-1204-5
https://doi.org/10.1038/s41586-019-1204-5
Autor:
Craig E. Manning, Stefano Poli, Antoine Boutier, Simone Tumiati, Laurent Remusat, Alberto Vitale Brovarone, Dimitri A. Sverjensky, Carla Tiraboschi
Publikováno v:
Goldschmidt2021 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::47075856a4083fdc312a237e607f9942
https://doi.org/10.7185/gold2021.5219
https://doi.org/10.7185/gold2021.5219
Autor:
Yumiko Harigane, Michael Kettermann, Manuel D. Menzel, Peter B. Kelemen, Juan Carlos de Obeso, Craig E. Manning, Alissa Kotowski, Ana Jesus, János Urai
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Hole BT1B of the Oman Drilling Project provides a continuous sampling from listvenite into the metamorphic sole that preserves the deformation, hydration and carbonation processes of oceanic mantle peridotite at the base of the Samail ophiolite, Oman
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fc300c01b53edd3fd2043e22dc5c838e
https://doi.org/10.1029/2020jb020199
https://doi.org/10.1029/2020jb020199