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1
Difference in keratinase activity of dermatophytes at different environmental conditions is an attribute of adaptation to parasitism
Difference in keratinase activity of dermatophytes at different environmental conditions is an attribute of adaptation to parasitism
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Difference in keratinase activity of dermatophytes at different environmental conditions is an attribute of adaptation to parasitism

Sharma, Anima ; Chandra, Subhash ; Sharma, Meenakshi

Mycoses, 2012-09, Vol.55 (5), p.410-415 [Revista revisada por pares]

Oxford, UK: Blackwell Publishing Ltd

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2
Recalcitrant soil organic materials mineralize more efficiently at higher temperatures
Recalcitrant soil organic materials mineralize more efficiently at higher temperatures
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Recalcitrant soil organic materials mineralize more efficiently at higher temperatures

Bol, Roland ; Bolger, Thomas ; Cully, Raymond ; Little, Declan

Journal of plant nutrition and soil science, 2003-06, Vol.166 (3), p.300-307 [Revista revisada por pares]

Weinheim: WILEY-VCH Verlag

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3
Anhydrous partial melting of MORB pyrolite and other peridotite compositions at 10 kbar: Implications for the origin of primitive MORB glasses
Anhydrous partial melting of MORB pyrolite and other peridotite compositions at 10 kbar: Implications for the origin of primitive MORB glasses
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Anhydrous partial melting of MORB pyrolite and other peridotite compositions at 10 kbar: Implications for the origin of primitive MORB glasses

FALLOON, T. J ; GREEN, D. H

Mineralogy and petrology, 1987-12, Vol.37 (3-4), p.181-219 [Revista revisada por pares]

New York: Springer

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4
Influence of Relative Humidity on the Crystallization of Fe(III) Oxides From Ferrihydrite
Influence of Relative Humidity on the Crystallization of Fe(III) Oxides From Ferrihydrite
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Influence of Relative Humidity on the Crystallization of Fe(III) Oxides From Ferrihydrite

Torrent, J.

Clays and clay minerals, 1982-01, Vol.30 (5), p.337-340 [Revista revisada por pares]

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5
Thermal Behavior of Hydrotalcite and of Anion-Exchanged Forms of Hydrotalcite
Thermal Behavior of Hydrotalcite and of Anion-Exchanged Forms of Hydrotalcite
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Thermal Behavior of Hydrotalcite and of Anion-Exchanged Forms of Hydrotalcite

Brindley, G. W.

Clays and clay minerals, 1980-01, Vol.28 (2), p.87-91 [Revista revisada por pares]

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6
Experiments on the Hydrothermal Formation of Calcium Zeolites
Experiments on the Hydrothermal Formation of Calcium Zeolites
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Experiments on the Hydrothermal Formation of Calcium Zeolites

Wirsching, Ulrike

Clays and clay minerals, 1981-01, Vol.29 (3), p.171-183 [Revista revisada por pares]

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7
Formation of Halloysite from Feldspar: Low Temperature, Artificial Weathering Versus Natural Weathering
Formation of Halloysite from Feldspar: Low Temperature, Artificial Weathering Versus Natural Weathering
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Formation of Halloysite from Feldspar: Low Temperature, Artificial Weathering Versus Natural Weathering

Parham, Walter E.

Clays and clay minerals, 1969-01, Vol.17 (1), p.13-22 [Revista revisada por pares]

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8
Kaolinite, Smectite, and K-Rectorite in Bentonites: Relation to Coal Rank at Tulameen, British Columbia
Kaolinite, Smectite, and K-Rectorite in Bentonites: Relation to Coal Rank at Tulameen, British Columbia
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Kaolinite, Smectite, and K-Rectorite in Bentonites: Relation to Coal Rank at Tulameen, British Columbia

Pevear, D. R.

Clays Clay Miner.; (United States), 1980-01, Vol.28 (4), p.241-254 [Revista revisada por pares]

United States

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9
Thermal Transformation of Antigorite as Studied by Electron-Optical Methods
Thermal Transformation of Antigorite as Studied by Electron-Optical Methods
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Thermal Transformation of Antigorite as Studied by Electron-Optical Methods

de Souza Santos, Helena

Clays and clay minerals, 1983-01, Vol.31 (4), p.241-250 [Revista revisada por pares]

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10
An Expansible Mineral Having High Rehydration Ability
An Expansible Mineral Having High Rehydration Ability
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An Expansible Mineral Having High Rehydration Ability

Tomita, Katsutoshi

Clays and clay minerals, 1973-01, Vol.21 (3), p.185-190, Article 185 [Revista revisada por pares]

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