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
en En
| MEDLINE
| ID: mdl-30091010
Palabras clave
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 datos:
MEDLINE
Asunto principal:
Agua
/
Planeta Tierra
/
Origen de la Vida
/
Minerales
Idioma:
En
Revista:
Orig Life Evol Biosph
Asunto de la revista:
BIOLOGIA
/
BIOLOGIA MOLECULAR
Año:
2018
Tipo del documento:
Article
País de afiliación:
Francia