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Aragonite, CaCC

SAQ 3.10 Calcite and aragonite are both forms of calcium carbonate, CaCC>3. Calcite converts to form aragonite. If A"f°(calcite) = -1206.92 kJ... [Pg.122]

Polymorph Two or more solid crystalline substances with the same chemistry, but different crystalline structures. Calcite (rhombohedral CaCCE) and aragonite (orthorhombic CaCCE) are polymorphs. [Pg.462]

Figure 2.1. Generalized phase relations in the unary system CaCC>3. "A" -aragonite "I" through "V - calcite polymorphs with metastable fields indicated by (). Dash-dot line at 800°C represents transition encountered on cooling runs solid line at lower T represents transition encountered on heating runs. (After Carlson, 1980.)... Figure 2.1. Generalized phase relations in the unary system CaCC>3. "A" -aragonite "I" through "V - calcite polymorphs with metastable fields indicated by (). Dash-dot line at 800°C represents transition encountered on cooling runs solid line at lower T represents transition encountered on heating runs. (After Carlson, 1980.)...
This model has the attractive characteristics of not requiring biotic or chemical formation of CaCC>3 directly on odid surfaces and offering an explanation for the observation that odids appear to require "rest" between depositional cycles. It also provides a reasonable explanation for the concentric organic-rich layers generally observed in laminated aragonitic odids. Researchers such as Oppenheimer (1961), Cloud (1962a), Wilson (1967), and Folk (1973) have accepted the general principles put forth in this model. [Pg.233]

Kinsman J.J. and Holland H. D. (1969) The coprecipitation of cations with CaCC>3-IV. The coprecipitation of Sr2+ with aragonite between 16° and 96°C. Geochim. Cosmochim. Acta 33, 1-17. [Pg.641]


See other pages where Aragonite, CaCC is mentioned: [Pg.246]    [Pg.246]    [Pg.120]    [Pg.302]    [Pg.134]    [Pg.153]    [Pg.153]    [Pg.248]    [Pg.355]    [Pg.409]    [Pg.621]    [Pg.44]    [Pg.146]    [Pg.424]   
See also in sourсe #XX -- [ Pg.3 , Pg.75 ]




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Aragonite

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