1985
DOI: 10.1016/0037-0738(85)90071-5
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Grain size of granite and derived grus, Enchanted Rock pluton, Texas

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Cited by 15 publications
(14 citation statements)
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“…The results of this research in small ephemeral granitic watersheds provide additional support for an "asymmetry in bedrock erodibility" (p. 464) facilitating strath development. Granite's tendency to break down into grus through biotite decay (Isherwood and Street, 1976;Hoskin and Sundeen, 1985), discongruent dissolution ( fig. 6), and biotic processes ( fig.…”
Section: Resultsmentioning
confidence: 99%
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“…The results of this research in small ephemeral granitic watersheds provide additional support for an "asymmetry in bedrock erodibility" (p. 464) facilitating strath development. Granite's tendency to break down into grus through biotite decay (Isherwood and Street, 1976;Hoskin and Sundeen, 1985), discongruent dissolution ( fig. 6), and biotic processes ( fig.…”
Section: Resultsmentioning
confidence: 99%
“…The premise is that the lack of grain-to-grain attachment promotes granular disintegration or grussification (Isherwood and Street, 1976;Hoskin and Sundeen, 1985). For each cobble studied, 100 sequential perimeter mineral grains were "cut out" digitally from the backscattered electron microscope (BSE) imagery of polished cross-sections.…”
Section: Hypotheses Of Strath Formationmentioning
confidence: 99%
“…This results in the development of microsheeting joints which run parallel to the weathering surface and cut indiscriminately across minerals causing grain-grain disaggregation. Subsequent observations by Hoskin and Sundeen (1985) have provided some support for this idea. Pye (1985) suggested that the first step in the breakdown of a granitoid rock mass would be granular disintegration due to the exploitation of weaknesses along mineral boundaries.…”
Section: Microfracture Initiation Within Weathering Profilesmentioning
confidence: 58%
“…The presence of these 'Moss Defects' within granitic quartz and their subsequent exploitation during the breakdown of granitoid parent rocks into grus may, at least partially, explain the lack of correspondence which Hoskin and Sundeen (1985) observed between the texture of parent granites and the grain size of the grus at Enchanted Rock, Texas. However, Power et al (1990) investigated the possibility that certain weathering processes may be sufficiently energetic to, not only exploit pre-existing structural flaws such as 'Moss Defects', but also initiate microfractures in previously sound quartz.…”
Section: Microfracture Initiation Within Weathering Profilesmentioning
confidence: 76%
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