Zusammenfassung
Auf der Insel Thera, im Attiko-Kykladishen Gürtel, ist ein Granitkörper in einer Tiefe von ca. 250 m durch eine Bohrung aufgedeckt. Dieser Granitkörper ist in metamorphen Gesteinen von Blauschiefer-Facies intrudiert. K-Ar-Biotit- und Ar-Ar-Feldspat-Altersbestimmungen streuen um 9.5 Ma. Diese Alter weisen auf rasche Abkühlung des Granitkörpers hin. Es zeigt sich somit, daß die thermometamorphe Entwicklung des Attiko-Kykladischen Gürtels bis zur Insel Thera reicht.
Abstract
A granite was drilled in the prevolcanic basement of Thera, an island of the Attico-Cycladic belt. It intruded the blueschist facies country rocks. K-Ar biotite ages and Ar-Ar plateau ages on two feldspars indicate rapid cooling, as all ages cluster around 9.5 Ma. Its occurrence indicates that the thermometamorphic evolution that characterizes the Attiko-Cycladic belt extends as far as Thera.
Résumé
Un forage a été pratiqué dans un granite du socle pré-volcanique de l'île de Thera, qui appartient à la ceinture attico-cycladique. Ce granite a intrudé les roches encaissantes de facies schistes bleus. Les datations effectuées sur les biotites par la méthode K-Ar et les âges-plateau des feldspaths obtenus par la méthode Ar-Ar indiquent un refroidissement rapide, puisque tous les âges sont de l'ordre de 9,5 Ma. Ce granite montre que l'évolution thermométamorphique qui caractérise la ceinture Attico-Cycladique s'étend jusqu'à l'île de Thera.
Краткое содержание
При бурении на остров е Thera в аттикокикладско м поясе установили на г лубине 250 м присутствие гранитн ого тела. Это тело интр удировано в метаморфические по роды фация голубого сланца. Иссл едования с помощью методов калия/аргона по биотитам и аргона/ аргона по полевым шпа там дали возраст этих пород примерно 9,5 ма. Эт о говорит о том, что охлаждение грани тного тела протекало довольно быстро. Т.о. уд алось показать, что термометаморфизм за хватывал и остров Thera.
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Skarpelis, N., Kyriakopoulos, K. & Villa, I. Occurrence and40Ar/39Ar dating of a granite in Thera (Santorini, Greece). Geol Rundsch 81, 729–735 (1992). https://doi.org/10.1007/BF01791388
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DOI: https://doi.org/10.1007/BF01791388