Water near its Supercritical Point and at Alkaline pH for the Production of Ferric Oxides and Silicates in Anoxic Conditions. A New Hypothesis for the Synthesis of Minerals Observed in Banded Iron Formations and for the Related Geobiotropic Chemistry inside Fluid Inclusions.
Orig Life Evol Biosph
; 48(3): 289-320, 2018 Sep.
Article
em En
| MEDLINE
| ID: mdl-30091010
Palavras-chave
Abiogenic ferric iron; Amino-acids; Amorphous silica; Anoxic iron oxidation; Banded Iron Formations; Ferric oxide hydroxides; Ferric oxides; Ferric silicates; Ferrous/ferric iron; Fluid inclusions; Geobiotropic chemistry; Geobiotropy; Geochemical origin of life; Hamersley Group; High pH; High-subcritical water; Prebiotic matter; Raman analysis; Theoretical & experimental work; Transvaal Supergroup
Texto completo:
1
Base de dados:
MEDLINE
Assunto principal:
Água
/
Planeta Terra
/
Origem da Vida
/
Minerais
Idioma:
En
Ano de publicação:
2018
Tipo de documento:
Article