Earth:Dacite

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Short description: Volcanic rock intermediate in composition between andesite and rhyolite
Dacite from the Western Carpathians

Dacite (/ˈdeɪsaɪt/) is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz.

Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline tholeiitic and calc-alkaline magma series.

Composition

Aphanitic QAPF diagram denoting dacite
TAS diagram with the dacite (O3) field highlighted in yellow

Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass.[1] The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form transitions to the rhyolites.[2]

The relative proportions of feldspars and quartz in dacite, and in many other volcanic rocks, are illustrated in the QAPF diagram. This defines dacite as having a content of 20% to 60% quartz, with plagioclase making up 65% or more of its feldspar content.[3][4][5][6] However, while the IUGS recommends classifying volcanic rocks on the basis of their mineral composition whenever possible, dacites are often so fine-grained that mineral identification is impractical. The rock must then be classified chemically based on its content of silica and alkali metal oxides (K2O plus Na2O). The TAS classification puts dacite in the O3 sector.

Texture

Grey, red, black, altered white/tan, flow-banded pumice dacite

In hand specimen, many of the hornblende and biotite dacites are grey or pale brown and yellow rocks with white feldspars, and black crystals of biotite and hornblende. Other dacites, especially pyroxene-bearing dacites, are darker colored.[2]

In thin section, dacites may have an aphanitic to porphyritic texture. Porphyritic dacites contain blocky highly zoned plagioclase phenocrysts and/or rounded corroded quartz phenocrysts. Subhedral hornblende and elongated biotite grains are present. Sanidine phenocrysts and augite (or enstatite) are found in some samples. The groundmass of these rocks is often aphanitic microcrystalline, with a web of minute feldspars mixed with interstitial grains of quartz or tridymite; but in many dacites it is largely vitreous, while in others it is felsitic or cryptocrystalline.

Geological context and formation

Thin section of a porphyritic dacite from Mount St. Helens

Dacite usually forms as an intrusive rock such as a dike or sill. Examples of this type of dacite outcrop are found in northwestern Montana and northeastern Bulgaria. Nevertheless, because of the moderately high silica content, dacitic magma is quite viscous[7] and therefore prone to explosive eruption. A notorious example of this is Mount St. Helens in which dacite domes formed from previous eruptions. Pyroclastic flows may also be of dacitic composition as is the case with the Fish Canyon Tuff of La Garita Caldera.[8]

Dacitic magma is formed by the subduction of young oceanic crust under a thick felsic continental plate. Oceanic crust is hydrothermally altered causing addition of quartz and sodium.[9] As the young, hot oceanic plate is subducted under continental crust, the subducted slab partially melts and interacts with the upper mantle through convection and dehydration reactions.[10] The process of subduction creates metamorphism in the subducting slab. When this slab reaches the mantle and initiates the dehydration reactions, minerals such as talc, serpentine, mica and amphiboles break down generating a more sodic melt.[11] The magma then continues to migrate upwards causing differentiation and becomes even more sodic and silicic as it rises. Once at the cold surface, the sodium rich magma crystallizes plagioclase, quartz and hornblende.[12] Accessory minerals like pyroxenes provide insight to the history of the magma.

The formation of dacite provides a great deal of information about the connection between oceanic crust and continental crust. It provides a model for the generation of felsic, buoyant, perennial rock from a mafic, dense, short-lived one.

Dacite's role in the formation of Archean continental crust

The process by which dacite forms has been used to explain the generation of continental crust during the Archean eon. At that time, the production of dacitic magma was more ubiquitous, due to the availability of young, hot oceanic crust. Today, the colder oceanic crust that subducts under most plates is not able to melt prior to the dehydration reactions, thus inhibiting the process.[13]

Molten dacite magma at Kīlauea

Dacitic magma was encountered in a drillhole during geothermal exploration on Kīlauea in 2005. At a depth of 2488 m, the magma flowed up the wellbore. This produced several kilograms of clear, colorless vitric (glassy, non-crystalline) cuttings at the surface. The dacite magma is a residual melt of the typical basalt magma of Kīlauea.[14]

Distribution

Dacite is relatively common and occurs in various tectonic and magmatic contexts:

  • In oceanic volcanic series. Examples: Iceland (Heiðarsporður ridge),[15] Juan de Fuca Ridge.[16]
  • In calc-alkaline and tholeiitic volcanic series of the subduction zones of island arcs and active continental margins. Examples of dacitic magmatism in island arcs are Japan , the Philippines , the Aleutians, the Antilles, the Sunda Arc (Mount Batur),[17] Tonga and the South Sandwich Islands. Examples of dacitic magmatism in active continental margins are the Cascade Range, Guatemala and the Andes (Ecuador and Chile ).
  • In continental volcanic series, often in association with tholeiitic basalts and intermediary rocks

The type locality of dacite is Gizella quarry near Poieni, Cluj in Romania.[18] Other occurrences of dacite in Europe are Germany (Weiselberg), Greece (Nisyros and Thera), Italy (in Bozen quartz porphyry, and Sardinia), Austria (Styrian Volcano Arc), Scotland (Argyll),[19] Slovakia, Spain (El Hoyazo near Almería),[20] France (Massif de l'Esterel)[21] and Hungary (Csódi Hill).[22]

Sites outside Europe include Iran, Morocco, New Zealand (volcanic region of Taupo), Turkey, United States and Zambia.[citation needed]

Dacite is found extraterrestrially at Nili Patera caldera of Syrtis Major Planum on Mars.[23]

Etymology

The word dacite comes from Dacia, a province of the Roman Empire which lay between the Danube River and Carpathian Mountains (now modern Romania and Moldova) where the rock was first described.[18]

The term dacite was used for the first time in the scientific literature in the book Geologie Siebenbürgens (The Geology of Transylvania) by Austrian geologists Franz Ritter von Hauer and Guido Stache.[18][24] Dacite was originally defined as a new rock type to separate calc-alkaline rocks with oligoclase phenocrysts (dacites) from rocks with orthoclase phenocrysts (rhyolites).[18]

See also

References

  1. ↑ Troll, Valentin R.; Donaldson, Colin H.; Emeleus, C. Henry. (2004-08-01). "Pre-eruptive magma mixing in ash-flow deposits of the Tertiary Rum Igneous Centre, Scotland" (in en). Contributions to Mineralogy and Petrology 147 (6): 722–739. doi:10.1007/s00410-004-0584-0. ISSN 1432-0967. Bibcode: 2004CoMP..147..722T. https://doi.org/10.1007/s00410-004-0584-0. 
  2. ↑ 2.0 2.1  One or more of the preceding sentences incorporates text from a publication now in the public domain: Flett, John Smith (1911). "Dacite". in Chisholm, Hugh. Encyclopædia Britannica. 7 (11th ed.). Cambridge University Press. p. 728. 
  3. ↑ Le Bas, M. J.; Streckeisen, A. L. (1991). "The IUGS systematics of igneous rocks". Journal of the Geological Society 148 (5): 825–833. doi:10.1144/gsjgs.148.5.0825. Bibcode: 1991JGSoc.148..825L. 
  4. ↑ "Rock Classification Scheme - Vol 1 - Igneous". British Geological Survey: Rock Classification Scheme 1: 1–52. 1999. http://nora.nerc.ac.uk/id/eprint/3223/1/RR99006.pdf. 
  5. ↑ "Classification of igneous rocks". http://geology.csupomona.edu/alert/igneous/igclass.htm. 
  6. ↑ Philpotts, Anthony R.; Ague, Jay J. (2009). Principles of igneous and metamorphic petrology (2nd ed.). Cambridge, UK: Cambridge University Press. pp. 139–143. ISBN 9780521880060. 
  7. ↑ Whittington, A. G.; Hellwig, B. M.; Behrens, H.; Joachim, B.; Stechern, A.; Vetere, F. (2009). "The viscosity of hydrous dacitic liquids: implications for the rheology of evolving silicic magmas". Bulletin of Volcanology 71 (2): 185–199. doi:10.1007/s00445-008-0217-y. Bibcode: 2009BVol...71..185W. 
  8. ↑ "Outflow ignimbrite sheet of Fish Canyon Tuff: crystal-rich dacitic ignimbrite erupted from La Garita caldera". USGS. http://pubs.usgs.gov/sim/3123/site/photos/10.pdf. 
  9. ↑ Devore, G. W. (1983). "The influence of submarine weathering of basalts on their partial melting during subduction". Lithos 16 (3): 203–213. doi:10.1016/0024-4937(83)90024-5. Bibcode: 1983Litho..16..203D. 
  10. ↑ Drummond, M. S.; Defant, M. J. (1990). "A model for Trondhjemite-Tonalite-Dacite Genesis and crustal growth via slab melting: Archean to modern comparisons". Journal of Geophysical Research 95 (B13): 21503–21521. doi:10.1029/JB095iB13p21503. Bibcode: 1990JGR....9521503D. 
  11. ↑ Fyfe, W.; McBirney, A. (1975). "Subduction and the structure of andesitic volcanic belts". American Journal of Science 275-A: 285–297. 
  12. ↑ Defant, M. J.; Richerson, P. M.; de Boer, J. Z.; Stewart, R. H.; Maury, R. C.; Bellon, H.; Drummond, M. S.; Feigenson, M. D. et al. (1991). "Dacite Genesis via both Slab Melting and Differentiation: Petrogenesis of La Yeguada Volcanic Complex, Panama". Journal of Petrology 32 (6): 1101–1142. doi:10.1093/petrology/32.6.1101. Bibcode: 1991JPet...32.1101D. 
  13. ↑ Atherton, M. P.; Petford, N. (1993). "Generation of sodium-rich magmas from newly underplated basaltic crust". Nature 362 (6416): 144–146. doi:10.1038/362144a0. Bibcode: 1993Natur.362..144A. 
  14. ↑ Puna Dacite Magma at Kilauea: Unexpected Drilling Into an Active Magma Posters, 2008 Eos Trans. AGU, 89(53), Fall Meeting
  15. ↑ Mancini, A.; Mattsson, H.B.; Bachmann, O. (2015). "Origin of the compositional diversity in the basalt-to-dacite series erupted along the Heiðarsporður ridge, NE Iceland". Journal of Volcanology and Geothermal Research 301: 116–127. doi:10.1016/j.jvolgeores.2015.05.010. Bibcode: 2015JVGR..301..116M. 
  16. ↑ Perfit, M.R.; Schmitt, A.K.; Ridley, W.I.; Rubin, K.H.; Valley, J.W. (2008). "Petrogenesis of dacites from the southern Juan de Fuca Ridge". Goldschmidt Conference 2008. https://www.academia.edu/24261994. Retrieved 23 February 2018. 
  17. ↑ Wheller, Graeme Eric (1986). Petrogenesis of Batur caldera, Bali, and the geochemistry of Sunda-Banda arc basalts (phd). PhD thesis, University of Tasmania.
  18. ↑ 18.0 18.1 18.2 18.3 Ştefan, Avram; Szakács, Alexandru; Seghedi, loan (June 1996). Dacite from type locality: Genealogy and description. Geological Survey of Romania. https://adatbank.ro/vendeg/htmlk/pdf6037.pdf. Retrieved 20 February 2022. 
  19. ↑ Ellis, R. A. (1977). lnvestigation of disseminated copper mineralisation near Kilmelford, Argyllshire, Scotland (Mineral Reconnaissance Programme Report 9). London: Institute of Geological Sciences. http://nora.nerc.ac.uk/id/eprint/10029/1/WFMR77009.pdf. 
  20. ↑ Acosta-Vigil, Antonio; Buick, Ian; Cesare, Bernardo; London, David; Morgan, VI, George B. (2012). "The Extent of Equilibration between Melt and Residuum during Regional Anatexis and its Implications for Differentiation of the Continental Crust: a Study of Partially Melted Metapelitic Enclaves". Journal of Petrology 53 (7): 1319–1356. doi:10.1093/petrology/egs018. Bibcode: 2012JPet...53.1319A. https://academic.oup.com/petrology/article/53/7/1319/1541445/The-Extent-of-Equilibration-between-Melt-and. 
  21. ↑ Thomas, Pierre (May 2016). "Dacite (Esterellite)" (in fr). Observer les objets géologiques. Lithothèque ENS de Lyon. http://lithotheque.ens-lyon.fr/Lithotheque/FormRech/page.php?recup=A18.7. 
  22. ↑ "Dacite". Hungarian Natural History Museum. http://publication.nhmus.hu/NatEu/HNHM_Exhibition/HNHM-EXH_kopark-19.pdf. 
  23. ↑ "Nili Patera and Dacite Lava Flow". Mars Exploration – Multimedia. NASA. 1 April 2012. https://mars.nasa.gov/multimedia/images/?ImageID=5298&s=5. 
  24. ↑ Ritter von Hauer, Franz; Stache, Guido (1863) (in de). Geologie Siebenbürgens. Vienna: Wilhelm Brauchmüller. p. 72. https://archive.org/details/bub_gb_CYwAAAAAcAAJ. "v. Richthofen's Namen gleichfalls ganz fallen zu lassen, dafür liegt wol nicht derselbe Grund vor. Dass die Oligoklasgruppe der "Quarztrachyte", dies muss der Name für die ganze Reihe bleiben, von der Orthoklasgruppe oder den "Rhyoliten" getrennt werden müsse, dafür plaidirte Roth gleichfalls schon in seiner Arbeit. Unser Nachweis der Altersverschiedenheit spricht nur um so dringender dafür. Für den Geologen genügen vielleicht die Namen "jüngerer" und "älterer" Quarztrachyt. Soll jedoch entsprechend der Sonderbezeichnung für die jüngere Gruppe, auch für die ältere Gruppe der Quarztrachyte ein besonderer Name eingeführt werden, so möchte der Name "Dacit" vielleicht entsprechend sein, da die Gruppe im alten Dacien eine besonders hervorragende Rolle zu spielen scheint)." 



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