Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Liberto de Pablo"'
Publikováno v:
American Mineralogist. 98:977-985
Cristobalite-tridymite blade nanocrystals cemented by SiO2-glass and tridymite nanocrystals fill separately SiO2-glass spherules released by explosive volcanism, in rhyolitic tuffs from the Province of the Mesa Central, Mexico. This paper presents th
Publikováno v:
Chemical Engineering Journal. 171:1276-1286
Adsorption of Hg 2+ , Cr 3+ , Pb 2+ , Cu 2+ , Zn 2+ , Ba 2+ , Ni 2+ , Mn 2+ , Cd 2+ , Ba 2+ and Ag + by Ca-montmorillonite from monocationic solutions followed second-order kinetics, attaining removals q e of Pb 2+ 6.187 × 10 2 , Hg 2+ 4.369 × 10 2
Publikováno v:
The Canadian Mineralogist. 45:281-292
Monte Carlo simulations in NP zz T and μVT ensembles of the hydration of Ca-saturated Wyoming-type montmorillonite show that one-layer Ca-exchanged montmorillonite hydrate with a d 001 of 12.11 A is stable at 353 K, 300 bar, and −7.21 kcal/mol pot
Publikováno v:
Langmuir. 21:10874-10884
Monte Carlo grand canonical molecular simulations on the hydration of Na-, K-, and Ca-montmorillonite show that between 333 and 533 K and 300-1300 bar Na-montmorillonite forms stable one-layer hydrates of d(001) spacings 12.64-12.38 Angstroms, K-mont
Publikováno v:
Langmuir. 20:10764-10770
Monte Carlo molecular simulations of the hydration of K-saturated Wyoming-type montmorillonite at constant stress in the NPzzT ensemble and at constant chemical potential in the grand canonical muVT ensemble, under basin-like conditions of 353 K and
Publikováno v:
Clays and Clay Minerals. 50:807-823
Diagenesis of the Holocene-Pleistocene volcanogenic sediments of the Mexican Basin produced, in strata of gravel and sand, 1H2O- and 2H2O-smectite, kaolinite, R3-2H2O-smectite (0.75)-kaolinite, R1-2H2O-smectite (0.75)-kaolinite, R3-kaolinite (0.75)-2
Autor:
Liberto de Pablo Galán, Leticia Rosales-Hoz, Arturo Carranza-Edwards, Gerardo Bocanegra-Garcı́a
Publikováno v:
Sedimentary Geology. 119:263-274
Fifty beach locations were sampled in Baja California Peninsula, Mexico, in order to characterize textural and compositional parameters. The western beach sands are mainly associated with a lower relief coastal plain and high energy of waves and curr
Publikováno v:
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.31
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scopus-Elsevier
UNAM
Redalyc-UNAM
Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.31
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scopus-Elsevier
This paper presents the occurrence, mineralogy and process of formation of CaK-clinoptilolite, KNa-chabazite, KNa-heulandite, KNa-erionite and Na-phillipsite in pyroclastic rocks from the Calvillo-Jalpa-Nochixtlán area in the Province of the Mesa Ce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7c818f57fd1601c753a33592b94ffae8
https://www.redalyc.org/articulo.oa?id=57231378009
https://www.redalyc.org/articulo.oa?id=57231378009
Publikováno v:
Physics and Chemistry of Minerals. 24:90-101
The electrical properties of opal-CT are validated at temperatures from 600 to 840 °C and frequencies from 5 Hz to 10 MHz. The opals are hydrothermal, containing less than 11270 ppm total of Al, Fe, Ca, Na, and K, and from 1.17 to 17.63 wt% H2O inte
Publikováno v:
Clays and Clay Minerals. 44:324-338
Sedimentary zeolites clinoptilolite, mordenite and erionite occur as diagenetic products of ash falls of rhyolitic composition from the Oligocene Chichindaro Formation at the limits of the Mexican Volcanic Belt with the Mexican Highland. These zeolit