Phacolith

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Cross-sectional diagram of phacoliths (red) in older folded rocks Phacolith.jpg
Cross-sectional diagram of phacoliths (red) in older folded rocks

A phacolith is a pluton of igneous rock parallel to the bedding plane or foliation of folded country rock. More specifically, it is a typically lens-shaped pluton that occupies either the crest of an anticline or the trough of a syncline. In rare cases the body may extend as a sill from the crest of an anticline through the trough of an adjacent syncline, such that in cross section it has an S shape. In intensely folded terrain the hinge of folds would be areas of reduced pressure and thus potential sites for magma migration and emplacement.

Contents

The term was coined and initially defined by Alfred Harker in his The Natural History of Igneous Rocks in 1909.

Examples

See also

References

  1. Baker, D.R.; Buddington, A.F. (1970). Geology and Magnetite Deposits of the Franklin Quadrangle and Part of the Hamburg Quadrangle, New Jersey (USGS Professional Paper 638) (PDF). Washington D.C.: USGS. p. 30.
  2. McCarthy, William; Reavy, R. John; Stevenson, Carl T.; Petronis, Michael S. (2015). "Late Caledonian transpression and the structural controls on pluton construction; new insights from the Omey Pluton, western Ireland" . Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 106 (1): 11–28. Bibcode:2015EESTR.106...11M. doi:10.1017/S1755691015000201. S2CID   132563143.
  3. Dasgupta, N.; Paljoydeep, T.; Ghosh, S. (2011). "Characteristics of pegmatoidal granite exposed near Bayalan, Ajmer district, Rajasthan". Journal of Earth System Science. 120 (4): 617–626. Bibcode:2011JESS..120..617D. doi: 10.1007/s12040-011-0100-7 .
  4. Leong, Goh Cheng (1995-10-27). Certificate Physics And Human Geography; Indian Edition. Oxford University Press. p. 21. ISBN   978-0-19-562816-6.
  5. Earp, J.R.; Hains, B.A. (1971). The Welsh Borderland. British Regional Geology (3rd ed.). London: Her Majesty’s Stationery Office.