Mineral Genesis
Definition
Mineral genesis addresses the questions of where, why, and how minerals form and disappear, on and in the Earth (see also Crystal Growth).
The Crystalline Earth and Its Dynamics
Minerals, essentially as natural crystals, are the major constituents of the core, the mantle, and the crust of our planet. In the mantle, they form the viscous solid matter involved in slow convective movements which act as the force-transmitting medium for plate tectonics. As such, minerals undergo phase transitions, polymorphic transitions, and more generally nucleation, growth as well as resorption. This occurs in response to local and/or temporal changes in pressure/stress, temperature, and chemical composition. Internal heat production of the Earth is ultimately the cause of mineral dynamics. Most active and diverse kinetic phenomena of these kinds are expected to take place where temperature gradients and chemical gradients are prominent, i.e., in and on the crust.
References
- Baronnet A (1982) Ostwald ripening in solution. The case of calcite and mica. Estud Geol 38:185–198Google Scholar
- Baronnet A (1984) Growth kinetics of the silicates. A review of basic concepts. Fortschr Mineral 62:187–232Google Scholar
- Bravais A (1866) Etudes Cristallographiques. Gauthier-Villars, ParisGoogle Scholar
- Burton WK, Cabrera N, Frank FC (1951) The growth of crystals and the equilibrium structure of their surfaces. Philos Trans R Soc Lond 243:299–358CrossRefGoogle Scholar
- Cölfen H, Antonietti M (2008) Mesocrystals and nonclassical crystallization. Wiley, Chichester, p 288CrossRefGoogle Scholar
- Cordier P, Leroux H (2008) Ce que disent les minéraux. Belin-Pour la science, ParisGoogle Scholar
- De Yoreo et al (2015) Crystallization by particle attachment in synthetic, biogenic, and geologic environment. Science 349(6247):aaa6760CrossRefGoogle Scholar
- Dekeyser W, Amelinckx S (1955) Les dislocations et la croissance des cristaux. Masson, ParisGoogle Scholar
- Donnay JDH, Harker D (1937) A new law of crystal morphology extending the law of Bravais. Am Mineral 22:446–467Google Scholar
- Garcia-Ruiz JM, Melero-Garcia E, Hyde ST (2009) Morphogenesis of self-assembled nanocrystalline materials of barium carbonate and silica. Science 323:362–365CrossRefGoogle Scholar
- Garcia-Ruiz JM, Nakouzi E, Kotopoulou E, Tamborino L, Steinbock O (2017) Biomimetic mineral self-organization from silica-rich spring waters. Sci Adv 3:e1602285CrossRefGoogle Scholar
- Grigor’ev DP (1965) Ontogeny of minerals. Israel Program for Scientific Translations, JerusalemGoogle Scholar
- Hartman P, Perdok WG (1955) On the relations between structure and morphology of crystals. Acta Crystallogr 8:49–52CrossRefGoogle Scholar
- Jambon A (1980) Isotopic fractionation: a kinetic model for crystals growing from silicate melts. Geochim Cosmochim Acta 44:1373–1380CrossRefGoogle Scholar
- Kirkpatrick RJ (1983) Theory of nucleation in silicate melts. Am Mineral 68:66–77Google Scholar
- Kirkpatrick RJ, Kuo LC, Melchior J (1981) Crystal growth in incongruently-melting compositions: programmed cooling experiments with diopside. Am Mineral 66:223–241Google Scholar
- Kostov I (1965) Crystal habit and mineral genesis. Bull Strasimir Dimitrov Inst Geol 14:33–49Google Scholar
- Kostov I, Kostov RI (1999) Crystal habit of minerals, Bulgarian academic monographs 1. Prof. Marin Drinov Academic Publishing House and Pensoft, Sofia, p 415Google Scholar
- Ostwald W (1897) Studien über die Bildung und Umwandlung fester Körper. Z Phys Chem 22:289–330Google Scholar
- Paquette J, Reeder RJ (1995) Relationship between surface structure, growth mechanism, and trace element incorporation in calcite. Geochim Cosmochim Acta 59:735–749CrossRefGoogle Scholar
- Stranski IN (1928) Zur Theorie der Kristallswachstums. Z Phys Chem A 136:259–278Google Scholar
- Sunagawa I (1977) Natural crystallization. J Cryst Growth 42:214–223CrossRefGoogle Scholar
- Sunagawa I (1984) Growth of crystals in Nature. In: Sunagawa I (ed) Materials science of the Earth’s interior. Terra Scientific Publication Company, Tokyo, pp 61–103Google Scholar
- Sunagawa I (1987) Morphology of Minerals. In: Sunagawa I (ed) Morphology of crystals: part B. Terra Scientific Publication Company, Tokyo, pp 509–587Google Scholar
- Welsch B, Faure F, Famin V, Baronnet A, Bachélery P (2013) Dendritic crystallization; a single process for all the textures of olivine in basalts? J Petrol 54(3):539–574CrossRefGoogle Scholar