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Volumn 31, Issue 3, 2008, Pages 302-308

Columnar joints in the Patiño formation sandstones, Eastern Paraguay: A dynamic interaction between dyke intrusion, quartz dissolution and cooling-induced fractures

Author keywords

[No Author keywords available]

Indexed keywords

AQUEOUS SOLUTION; COOLING; DIKE; DISSOLUTION; FRACTURE MECHANICS; HEAT SOURCE; IGNEOUS INTRUSION; JOINT; POROSITY; QUARTZ; SANDSTONE; THERMAL EXPANSION;

EID: 55149121630     PISSN: 07053797     EISSN: None     Source Type: Journal    
DOI: 10.18814/epiiugs/2008/v31i3/003     Document Type: Article
Times cited : (9)

References (24)
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  • 2
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  • 3
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    • Berrocal, J., and Fernandes, C., 1996, Seismicity in Paraguay and neighbouring regions, in Comin-Chiaramonti, P., and Gomes, C. B., eds., Alkaline magmatism in central-eastem Paraguay. Relationships with coeval magmatism in Brazil: São Paulo, Edusp/Fapesp, pp. 57-66.
  • 5
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    • Some observations on the crystallization of amorphous silica
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    • Chen, C. T. and Marshall, W. L., 1982, Amorphous silica solubilities. Behavior in pure water and aqueous sodium chloride, sodium sulfate, magnesium chloride, and magnesium sulfate up to 350°C: Geochimica et Cosmochimica Acta, v. 46, pp. 279-287.
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    • Chen, C.T.1    Marshall, W.L.2
  • 12
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    • Fournier, R.O.1
  • 13
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    • Fournier, R. O. and Potter, R. W. I., 1982, An equation correlating the solubility of quartz in water from 25°to 900°C at pressures up to 10,000 bars: Geochimica et Cosmochimica Acta, v. 46, pp. 1969-1973.
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  • 14
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  • 15
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  • 16
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  • 23
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.