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Harley, S. L. (1989) The origins of granulites: a metamorphic perspective. Geological Magazine, 126 (3) 215-247 doi:10.1017/s0016756800022330

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Reference TypeJournal (article/letter/editorial)
TitleThe origins of granulites: a metamorphic perspective
JournalGeological Magazine
AuthorsHarley, S. L.Author
Year1989 (May)Volume126
Page(s)215-247Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800022330Search in ResearchGate
Mindat Ref. ID254193Long-form Identifiermindat:1:5:254193:2
GUID3e272154-9573-44a6-aec6-f4c5f8b88213
Full ReferenceHarley, S. L. (1989) The origins of granulites: a metamorphic perspective. Geological Magazine, 126 (3) 215-247 doi:10.1017/s0016756800022330
Plain TextHarley, S. L. (1989) The origins of granulites: a metamorphic perspective. Geological Magazine, 126 (3) 215-247 doi:10.1017/s0016756800022330
In(1989, May) Geological Magazine Vol. 126 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractAlthough many recent reviews emphasize a uniformity in granulite pressure–temperature (P–T) conditions and paths, granulites in reality preserve a spectrum of important petrogenetic features which indicate diversity in their modes of formation. A thorough survey of over 90 granulite terranes or occurrences reveals that over 50% of them record P–T conditions outside the 7.5 ± 1 kbar and 800 ± 50 °C average granulite regime preferred by many authors. In particular, an increasing number of very high temperature (900−1000 °C) terranes are being recognized, both on the basis of distinctive mineral assemblages and geothermobarometry. Petrogenetic grid and geothermobarometric approaches to the determination and interpretation of P–T histories are both evaluated within the context of reaction textures to demonstrate that the large range in P–T conditions is indeed real, and that both near-isothermal decompression (ITD) and near-isobaric cooling (IBC) P–T paths are important. Amphibolite–granulite transitions promoted by the passage of CO2-rich fluids, as observed in southern India and Sri Lanka, are exceptional and not representative of fluid-related processes in the majority of terranes. It is considered, on the contrary, that fluid-absent conditions are typical of most granulites at or near the time of their recorded thermal maxima.ITD granulites are interpreted to have formed in crust thickened by collision, with magmatic additions being an important extra heat source. Erosion alone is not, however, considered to be the dominant post-collisional thinning process. Instead, the ITD paths are generated during more rapid thinning (1−2 mm/yr exposure) related to tectonic exhumation during moderate-rate or waning extension. IBC granulites may have formed in a variety of settings. Those which show anticlockwise P–T histories are interpreted to have formed in and beneath areas of voluminous magmatic accretion, with or without additional crustal extension. IBC granulites at shallow levels (< 5 kbar) may also be formed during extension of normal thickness crust, but deeper-level IBC requires more complex models. Many granulites exhibiting IBC at deep crustal levels may have formed in thickened crust which underwent very rapid (5 mm/yr) extensional thinning subsequent to collision. It is suggested that the preservation of IBC paths rather than ITD paths in many granulites is primarily related to the rate and timescale of extensional thinning of thickened crust, and that hybrid ITD to IBC paths should also be observed.Most IBC granulites, and probably many ITD granulites, have not been exposed at the Earth's surface as a result of the tectonic episodes which produced them, but have resided in the middle and lower crust for long periods of time (100−2000 Ma) following these events. The eventual exhumation of most granulite terranes only occur through their incorporation in later tectonic and magmatic events unrelated to their formation.

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Waters (1985) Transactions of the Geological Society of South Africa 88, 323
Goldsmith (1977) American Mineralogist 62, 1063
()
England (1986) Collisional Tectonics 19, 83
Harris (1984) American Mineralogist 69, 1036
Bertrand (1989) Comptes Rendus de l' Academie des Sciences
Griffin (1986) The Nature of the Lower Continental Crust 24, 363
Green (1987) Magmatic Processes – Physiochemical Principles 1, 139
England (1987) Tectonic Settings of Regional Metamorphisms , 3
Touret (1986) The Nature of the Lower Continental Crust , 161
Sonder (1987) Continental Extensional Tectonics , 187
Sills (1987) Evolution of the Lewisian and Comparable Precambrian High Grade Terrains , 81
()
Ellis (1983) Antarctic Geoscience , 20
Newton (1982) American Mineralogist 67, 203
Dahl (1980) American Mineralogist 65, 852
Coolen (1980) GUA (Amsterdam) Paper 13, 1
Nantel (1978) Réunion Annuelle des Sciences de la Terre 6, 1
Maboko () Evolution of Metamorphic Belts
Sills (1984) Schweizerische Mineralogishe Petrographishe Mitteilung 64, 169
Sheraton (1980) Journal of the Geological Society of Australia 27, 305
Bohlen (1983) American Mineralogist 68, 1049
Lindsley (1983) American Mineralogist 68, 477
Lal (1984) Neues Jahrbuch für Mineralogie Monatshefte 150, 121
Sandiford (1986) American Mineralogist 71, 946
Not Yet Imported: Bulletin de la Société Géologique de France - journal-article : 10.2113/gssgfbull.S7-XVIII.4.1023

If you would like this item imported into the Digital Library, please contact us quoting Journal ID 10845
Not Yet Imported: Geophysical Monograph Series - book-chapter : 10.1029/GM014p0303

If you would like this item imported into the Digital Library, please contact us quoting Journal ID
Indares (1984) American Mineralogist 70, 272
Huckenholz (1981) Neues Jahrbuch für Mineralogie Abhandlungen 142, 223
Hormann (1980) Geological Survey of Finland Bulletin 308, 1
()


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