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pro vyhledávání: '"Zachary F. M. Burton"'
Autor:
Zachary F. M. Burton, Tim McHargue, Christopher H. Kremer, Roger B. Bloch, Jared T. Gooley, Chayawan Jaikla, Jake Harrington, Stephan A. Graham
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-8 (2023)
Abstract The early Eocene (~ 56–48 million years ago) was marked by peak Cenozoic warmth and sea levels, high CO2, and largely ice-free conditions. This time has been described as a period of increased continental erosion and silicate weathering. H
Externí odkaz:
https://doaj.org/article/467960b2de2247a3869b374f9341d65a
Autor:
Zachary F. M. Burton
Publikováno v:
Fuels, Vol 3, Iss 4, Pp 580-587 (2022)
Recent advances in basin and petroleum system modelling have allowed for the investigation of gas hydrate systems, including modelling of the generation, migration, and accumulation of biogenic and thermogenic gas within gas hydrate deposits. In this
Externí odkaz:
https://doaj.org/article/39799e9ffd4a4105882200621a49927d
Autor:
Zachary F. M. Burton, Laura N. Dafov
Publikováno v:
Fuels, Vol 3, Iss 3, Pp 555-562 (2022)
Gas hydrates comprise one of the largest reservoirs of organic carbon on Earth. Marine gas hydrate predominantly consists of biogenic (i.e., microbially generated) methane molecules trapped within lattice-like cages of frozen water molecules. Sedimen
Externí odkaz:
https://doaj.org/article/25c582fbdcea4a5dabac5277f2651d81
Autor:
Zachary F. M. Burton, Laura N. Dafov
Publikováno v:
Geochemistry, Geophysics, Geosystems. 24
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea3aed197062ee1c8d00ad07d57edc17
https://doi.org/10.1029/2022gc010704
https://doi.org/10.1029/2022gc010704