| Reference Type | Journal (article/letter/editorial) |
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| Title | Experimental investigation of clogging of fissures and pores in granite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Bourg, A. C. M. | Author |
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| Oustrière, P. | Author |
| Sureau, J. F. | Author |
| Year | 1985 (April) | Volume | 49 |
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| Issue | 351 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_49/49-351-223.pdf+ |
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| DOI | doi:10.1180/minmag.1985.049.351.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3727 | Long-form Identifier | mindat:1:5:3727:7 |
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| GUID | 0 |
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| Full Reference | Bourg, A. C. M., Oustrière, P., Sureau, J. F. (1985) Experimental investigation of clogging of fissures and pores in granite. Mineralogical Magazine, 49 (351) 223-231 doi:10.1180/minmag.1985.049.351.09 |
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| Plain Text | Bourg, A. C. M., Oustrière, P., Sureau, J. F. (1985) Experimental investigation of clogging of fissures and pores in granite. Mineralogical Magazine, 49 (351) 223-231 doi:10.1180/minmag.1985.049.351.09 |
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| In | (1985, April) Mineralogical Magazine Vol. 49 (351) Mineralogical Society |
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| Abstract/Notes | AbstractFluid flow through a fractured granite core and leaching experiments on granite powder (at constant temperatures of 50 and 100°C and during cooling from 100 to 50°C) indicate that the dissolved silica content of the fluids originates from the dissolution of feldspars and phyllosilicates. The dissolution of quartz is not ruled out but it should be a minor phenomenon. The precipitation of quartz may control the dissolved Si content during constant temperature leaching. During cooling from 100 to 50°C chalcedony, alumino-silicates, and chlorite are all capable of precipitation, possibly leading to some clogging or sealing of fissures. |
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