CoChat
Sign Up
Cited by 59Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisGeological and Geophysical Studies

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

A model for continental crust genesis by arc accretion: rare earth element evidence from the Irish Caledonides

Draut, Amy E, Clift, Peter D, Hannigan, Robyn E, Layne, Graham, Shimizu, Nobumichi·2002·Earth and Planetary Science Letters
DOI 10.1016/s0012-821x(02)00931-7
Open this paper in CoChat — free account

Overview

Integrity signals

Registry

Crossref · 10.1016/s0012-821x(02)00931-7

Cites

1 of 1 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Verification

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • Draut et al. [2002] demonstrate, using an example from the Paleozoic Caledonides, that the accretion process itself is fundamental in transforming the bulk chemistry of igneous arc crust into a suitable building block for the continental crust.

    “However, Draut et al. [2002] now demonstrate, using an example from the Paleozoic Caledonides, that the accretion process itself is fundamental in transforming the bulk chemistry of igneous arc crust into a suitable building block for the continental crust.”

    From Controls on tectonic accretion versus erosion in subduction zones: Implications for the origin and recycling of the continental crust (2004) · cites this paper as Draut et al., 2002

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 58

  1. S.R. Taylor, S.M., McLennan, The Continental Crust: its Composition and Evolution, Blackwell, Oxford, 1985, 312 pp.
  2. Ellam, 1988, Is average continental crust generated at subduction zones?, Geology, 16, 314, 10.1130/0091-7613(1988)016<0314:IACCGA>2.3.CO;2 · DOI · Paper page
  3. Davidson, 1996, Deciphering mantle and crustal signatures in subduction zone magmatism, Geophys. Monogr., 96, 251
  4. Taylor, 1967, The origin and growth of continents, Tectonophysics, 4, 17, 10.1016/0040-1951(67)90056-X · DOI
  5. Taylor, 1981, The composition and evolution of the continental crust: rare earth element evidence from sedimentary rocks, Philos. Trans. R. Soc. Lond., A301, 381, 10.1098/rsta.1981.0119 · DOI
  6. Christensen, 1995, Seismic velocity structure and composition of the continental crust; a global view, J. Geophys. Res., 100, 9761, 10.1029/95JB00259 · DOI · Paper page
  7. Bryan, 1972, Geology, petrography, and geochemistry of the Volcanic Islands of Tonga, J. Geophys. Res., 77, 1566, 10.1029/JB077i008p01566 · DOI
  8. Ewart, 1987, The Pleistocene-recent Tonga-Kermadec Arc lavas; interpretation of new isotopic and rare earth data in terms of a depleted mantle source model, J. Pet., 28, 495, 10.1093/petrology/28.3.495 · DOI · Paper page
  9. Holbrook, 1999, Structure and composition of the Aleutian island arc and implications for continental crust growth, Geology, 27, 31, 10.1130/0091-7613(1999)027<0031:SACOTA>2.3.CO;2 · DOI · Paper page
  10. Suyehiro, 1996, Continental crust, crustal underplating, and low-Q upper mantle beneath an oceanic island arc, Science, 272, 390, 10.1126/science.272.5260.390 · DOI · Paper page
  11. Pearcy, 1990, Mass balance calculations for two sections of island arc and implications for the formation of continents, Earth Planet. Sci. Lett., 96, 427, 10.1016/0012-821X(90)90018-S · DOI
  12. Miller, 1994, Seismic signature and geochemistry of an island arc: a multidisciplinary study of the Kohistan accreted terrane, northern Pakistan, J. Geophys. Res., 99, 11623, 10.1029/94JB00059 · DOI
  13. DeBari, 1989, Examination of the deep levels of an island arc: evidence from the Tonsina ultramafic-mafic assemblage, Tonsina, Alaska, J. Geophys. Res., 94, 4373, 10.1029/JB094iB04p04373 · DOI
  14. Jull, 2001, On the conditions for lower crustal convective instability, J. Geophys. Res., 106, 6423, 10.1029/2000JB900357 · DOI
  15. Friedrich, 1999, Geochronological constraints on the magmatic, metamorphic, and thermal evolution of the Connemara Caledonides, western Ireland, J. Geol. Soc. Lond., 156, 1217, 10.1144/gsjgs.156.6.1217 · DOI
  16. McKerrow, 1991, The Ordovician and Silurian development of the Iapetus Ocean, Spec. Pap. Paleontol., 44, 165
  17. Dewey, 1990, The Ordovician Evolution of the South Mayo Trough, western Ireland, Tectonics, 9, 887, 10.1029/TC009i004p00887 · DOI
  18. C.R. Van Staal, J.F. Dewey, C. MacNiocaill, W.S. McKerrow, The Cambrian-Silurian tectonic evolution of the northern Appalachians and British Caledonides: history of a complex, west and southwest Pacific-type segment of Iapetus, in: D.J. Blundell, A.C. Scott, (Eds.), Lyell: the Past is the Key to the Present, Geol. Soc. Lond. Spec. Pub. 143, 1998, pp. 199–242. · DOI
  19. A.L. Harris, P.J. Haselock, M.J. Kennedy, J.R. Mendum, C.B. Long, J.A. Winchester, P.W.G. Tanner, The Dalradian Supergroup in Scotland, Shetland and Ireland, in: W. Gibbons, A.L. Harris (Eds.), A Revised Correlation of Precambrian Rocks in the British Isles, Geol. Soc. Lond. Spec. Rep. 22, 1994, pp. 33–53. · DOI
  20. Yardley, 1976, Deformation and metamorphism of Dalradian rocks and evolution of the Connemara Cordillera, J. Geol. Soc. Lond., 132, 521, 10.1144/gsjgs.132.5.0521 · DOI
  21. Senior, 1978, Regional metasomatism and the geochemistry of the Dalradian metasediments of Connemara, western Ireland, J. Petrol., 19, 585, 10.1093/petrology/19.3.585 · DOI
  22. Leake, 1989, The metagabbros, orthogneisses and paragneisses of the Connemara complex, western Ireland, J. Geol. Soc. Lond., 146, 575, 10.1144/gsjgs.146.4.0575 · DOI
  23. Ryan, 1980, The stratigraphy and petrochemistry of the Lough Nafooey Group (Tremadocian), western Ireland, J. Geol. Soc. Lond., 137, 443, 10.1144/gsjgs.137.4.0443 · DOI
  24. Draut, 2001, Geochemical evolution of arc magmatism during arc-continent collision, South Mayo, Ireland, Geology, 29, 543, 10.1130/0091-7613(2001)029<0543:GEOAMD>2.0.CO;2 · DOI · Paper page
  25. Leake, 1983, Major southward thrusting of the Dalradian rocks of Connemara, western Ireland, Nature, 305, 210, 10.1038/305210a0 · DOI
  26. Cliff, 1996, U-Pb and Rb-Sr geochronology of magmatism and metamorphism in the Dalradian of Connemara, western Ireland, J. Geol. Soc. Lond., 153, 109, 10.1144/gsjgs.153.1.0109 · DOI
  27. Tucker, 1995, Early Paleozoic chronology: a review in light of new U-Pb zircon ages from Newfoundland and Britain, Can. J. Earth Sci., 32, 368, 10.1139/e95-032 · DOI
  28. Clift, 1994, Geochemical evolution of an Ordovician island arc, South Mayo, Ireland, J. Geol. Soc. Lond., 151, 329, 10.1144/gsjgs.151.2.0329 · DOI
  29. Leake, 1986, The geology of SW Connemara, Ireland; a fold and thrust Dalradian and metagabbroic-gneiss complex, J. Geol. Soc. Lond., 143, 221, 10.1144/gsjgs.143.2.0221 · DOI
  30. Hart, 1993, Experimental clinopyroxene/melt partitioning of 24 trace elements, Cont. Min. Pet., 113, 1, 10.1007/BF00320827 · DOI
  31. S.-s. Sun, W.F. McDonough, Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes, in: A.D. Saunders, M.J. Norry, (Eds.), Magmatism in the Ocean Basins, Geol. Soc. Spec. Pub. 42, 1989, pp. 313–345. · DOI
  32. Jagger, 1988, U-Pb ages of basic rocks and gneisses intruded into the Dalradian rocks of Cashel, Connemara, W. Ireland, J. Geol. Soc. Lond., 145, 645, 10.1144/gsjgs.145.4.0645 · DOI
  33. O’Nions, 1983, A neodymium isotope investigation of sediments related to crustal development in the British Isles, Earth Planet. Sci. Lett., 63, 229, 10.1016/0012-821X(83)90039-0 · DOI · Paper page
  34. M.D. Jagger, The Cashel District of Connemara, Co. Galway, Eire: An Isotopic Study, Ph.D. Thesis, University of Glasgow, Glasgow, 1985.
  35. Hanson, 1980, Rare earth elements in petrogenetic studies of igneous systems, Annu. Rev. Earth Planet. Sci. Lett., 8, 371, 10.1146/annurev.ea.08.050180.002103 · DOI
  36. Fujimaki, 1984, Partition coefficients of Hf, Zr, and REE between phenocrysts and groundmasses, proceedings of the fourteenth lunar and planetary science conference, part 2., J. Geophys. Res., 89, 662, 10.1029/JB089iS02p0B662 · DOI
  37. Kay, 1991, Creation and destruction of lower continental crust, Geol. Rundsch., 80, 259, 10.1007/BF01829365 · DOI
  38. Kay, 1993, Delamination and delamination magmatism, Tectonophysics, 219, 177, 10.1016/0040-1951(93)90295-U · DOI
  39. Arndt, 1989, An open boundary between lower continental crust and mantle; its role in crust formation and crustal recycling, Tectonophysics, 161, 201, 10.1016/0040-1951(89)90154-6 · DOI
  40. Nelson, 1991, A unified view of craton evolution motivated by recent deep seismic reflection and refraction results, Geol. J. Int., 105, 25
  41. Bird, 1978, Initiation of intracontinental subduction in the Himalaya, J. Geophys. Res., 83, 4975, 10.1029/JB083iB10p04975 · DOI
  42. Richardson, 1979, Metamorphic consequences of crustal eclogite production in overthrust orogenic zones, Earth Planet, Sci. Lett., 42, 183
  43. Dewey, 1988, The extensional collapse of orogens, Tectonics, 7, 1123, 10.1029/TC007i006p01123 · DOI · Paper page
  44. Kay, 1994, Young mafic back arc volcanic rocks as indicators of continental lithospheric delamination beneath the Argentine Puna plateau, central Andes, J. Geophys. Res., 99, 24323, 10.1029/94JB00896 · DOI
  45. Kohlstedt, 1995, Strength of the lithosphere: Constraints imposed by laboratory experiments, J. Geophys. Res., 100, 17587, 10.1029/95JB01460 · DOI · Paper page
  46. J.F. Dewey, P.D. Ryan, T.B. Andersen, Orogenic uplift and collapse, crustal thickness, fabrics and metamorphic phase changes: the role of eclogites, in: H.M. Prichard, T. Alabaster, N.B.W. Harris, C.R. Neary (Eds.), Magmatic Processes and Plate Tectonics, Geol. Soc. Spec. Pub. 76, 1993, pp. 325–343. · DOI
  47. Teng, 1996, Extensional collapse of the northern Taiwan mountain belt, Geology, 24, 949, 10.1130/0091-7613(1996)024<0949:ECOTNT>2.3.CO;2 · DOI · Paper page
  48. Wellings, 1998, Timing of deformation associated with the syn-tectonic Dawros-Currywongaun-Doughruagh Complex, NW Connemara, western Ireland, J. Geol. Soc. Lond., 155, 25, 10.1144/gsjgs.155.1.0025 · DOI
  49. Williams, 1989, Low-angle extensional faulting and the emplacement of the Connemara Dalradian, Ireland, Tectonics, 8, 427, 10.1029/TC008i002p00417 · DOI
  50. J.F. Dewey, M. Mange, Petrology of Ordovician and Silurian sediments in the Western Irish Caledonides: tracers of short-lived Ordovician continent-arc collision orogeny and the evolution of the Laurentian Appalachian-Caledonian margin, in: C. MacNiocall, P. Ryan (Eds.), Continental Tectonics, Geol. Soc. Spec. Pub. 164, 1999, pp. 55–107. · DOI
  51. Klemperer, 1991, A deep seismic reflection transect across the Irish Caledonides, J. Geol. Soc. Lond., 148, 149, 10.1144/gsjgs.148.1.0149 · DOI
  52. Ducea, 1998, A case for delamination of the deep batholithic crust beneath the Sierra Nevada, California, Int. Geol. Rev., 40, 78, 10.1080/00206819809465199 · DOI
  53. Manley, 2000, Timing of volcanism in the Sierra Nevada of California: evidence for Pliocene delamination of the batholithic root?, Geology, 28, 811, 10.1130/0091-7613(2000)28<811:TOVITS>2.0.CO;2 · DOI
  54. Draut, 2002, The origin and significance of the Delaney Dome Formation, Connemara, Ireland, J. Geol. Soc. Lond., 159, 95, 10.1144/0016-764901034 · DOI
  55. Herren, 1987, Zanskar shear zone northeast-southwest extension within the Higher Himalayas (Ladakh, India), Geology, 15, 409, 10.1130/0091-7613(1987)15<409:ZSZNEW>2.0.CO;2 · DOI · Paper page
  56. Hodges, 1992, Simultaneous Miocene extension and shortening in the Himalayan Orogen, Science, 258, 1466, 10.1126/science.258.5087.1466 · DOI
  57. Wang, 1999, Post-collisional magmatism around northern Taiwan and its relation with opening of the Okinawa Trough, Tectonophysics, 308, 363, 10.1016/S0040-1951(99)00111-0 · DOI
  58. P.D. Clift, H. Schouten, A.E. Draut, A general model of arc-continent collision and subduction polarity reversal from Taiwan and the Irish Caledonides, in: R. Larter, P. Leat (Eds.), Geol. Soc. London Spec. Publ., in press. · DOI

Cited by

Sorted by citations

Metadata

Authors
Draut, A. E., Clift, P. D., Hannigan, R. E., Layne, G., & Shimizu, N.
Affiliations
  • Woods Hole Oceanographic Institution (US)
  • Arkansas State University (US)
ORCID
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2002-11
Volume
203
Issue
3-4
Pages
861-877
ISSN
0012-821X (ISSN-L)
DOI
10.1016/s0012-821x(02)00931-7
OpenAlex
W2007137970
Cited by
59
References
1
Citations by year
2026: 1 · 2024: 1 · 2023: 1 · 2022: 3 · 2021: 2 · 2020: 1 · 2019: 2 · 2017: 1 · 2016: 4 · 2015: 2 · 2014: 4 · 2013: 2 · 2012: 2
FWCI
2.70
Type
journal article
Language
en
Open access
closed
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • Civil War Book Review (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
Keywords
arc magmatism, arc-continent collision, rare earth elements, light rare earth elements, Connemara, Dalradian, rhyolite, gabbro, diorite, fractional crystallization, crustal contamination

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review