"Troodos: A Giant Serpentinite Diapir"
written by Roelof Dirk Schuiling,
published by International Journal of Geosciences, Vol.2 No.2, 2011
has been cited by the following article(s):
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[1] مدلسازی پتانسیل معدنی ذخایر کرومیت تیپ انبانه ای با استفاده از نقشه های شاهد وزندار پیوسته در کمربند افیولیتی سبزوار‎
[2] A Timanian island-arc fragment in North Greenland: The Midtkap igneous suite
Journal of Geodynamics, 2018
[3] Petrogenesis of boninitic lavas from the Troodos Ophiolite, and comparison with Izu–Bonin–Mariana fore-arc crust
Earth and Planetary Science Letters, 2018
[4] Tracking the Serpentinite Feet of the Mediterranean Salt Giant
Geosciences, 2018
[5] From ocean depths to mountain tops: Uplift of the Troodos ophiolite (Cyprus) constrained by low‐temperature thermochronology and geomorphic analysis
Tectonics, 2016
[6] Hydrothermale Lagerstätten
Die Welt der Rohstoffe, 2016
[7] The Hyblean xenolith suite (Sicily): an unexpected legacy of the Ionian–Tethys realm
International Journal of Earth Sciences, 2015
[8] Modelling the long‐term deformation of the sedimentary substrate of Mt. Etna volcano (Italy)
Terra Nova, 2015
[9] Reply to “Comment on Manuella et al.'The Hyblean xenolith suite (Sicily): an unexpected legacy of the Ionian–Tethys realm'by Beccaluva et al.(2015)”
International Journal of Earth Sciences, 2015
[10] New evidence for Late Quaternary deformation of the substratum of Mt. Etna volcano (Sicily, Italy): clues indicate active crustal doming
Bulletin of Volcanology, 2014
[11] Neoproterozoic Cana Brava chrysotile deposit (Goiás, Brazil): Geology and geochemistry of chrysotile vein formation
Lithos, 2014
[12] Hydrothermale Lagerst?tten
Die Welt der Rohstoffe, 2014