Zurück zur Übersicht. Export RIS. Petrogenesis of Triassic and Cretaceous metamorphic rocks from Khanom Peninsular Thailand. Bernhard Neugschwentner. Art der Arbeit. Fakultät für Geowissenschaften, Geographie und Astronomie. Studiumsbezeichnung bzw. Universitätlehrgang ULG. Link zu u:search Print-Exemplar eventuell in Bibliothek verfügbar. Abstract Deutsch. Thailand besteht geologisch aus zwei Krustenblöcken, die ihren Ursprung in Gondwana haben. Sibumasu im Westen und Indochina im Osten. Dazwischen liegen die Inthanon-Zone und der Sukhothai-Arc Gürtel. Während dieses Modell für den Norden des Landes etabliert wurde und mittlerweile gut akzeptiert ist, ist seine Fortsetzung nach Süden immer noch umstritten. Daher wurde der Khanom Komplex untersucht, ein polymetamorpher Komplex auf der Halbinsel Thailands, SE von Surat Thani, der erstmals von Kosuwan beschrieben wurde. Er enthält Gneise, Schiefer, Calcsilikate, Marmor und wird von postorogenen Graniten durchschnitten. Ziel war es klar zu stellen, ob diese Gesteine eine ähnliche Geschichte wie die hochgradig are first and khao dating Gesteine im Norden des Landes haben oder nicht. Petrologische Untersuchungen in Kombination mit geochronologischen Untersuchungen wurden an zwei Gneisen in diesem Gebiet durchgeführt Haad Nai Phlao Gneis und Laem Thong Yang Gneisum den Zeitpunkt, die metamorphen Bedingungen und die tektonische Entwicklung der Halbinsel Thailands besser zu verstehen. Diese Gneise bestehen hauptsächlich aus Feldspat, Quarz und zwei Glimmern. Granat und Aluminosilicat, welche von Kosuwan beschrieben wurden, konnten nicht gefunden werden. Die Ergebnisse dieser Studie legen nahe, dass der amphibolhaltige Gneis möglicherweise aus dem Khao Dat Fa Granit stammt und dass der Haad Nai Phlao Gneis das Ergebnis einer Kontaktmetamorphose ist, die durch das Eindringen des Khao Pret-Granits verursacht wird. Ähnliche Alter, welche in anderen metamorphen Gesteinen in Thailand gemessen wurden z. Abstract Englisch. Thailand is part of two main terranes which have their origins in the Gondwana continent, Sibumasu in the west and Indochina in the east. In between are the Inthanon Zone and the Sukhothai arc belt. Whereas this model was established for the northern part of the country and is now well accepted, its continuation to the south is still a matter of debate. Therefore the Khanom complex, a polymetamorphic complex located in Peninsular Thailand SE of Surat Thani first described by Kosuwan was examined. It contains gneisses, schists, calcsilicates, marbles and is crosscut by postorogenic granites. The objective was to bring more clarity whether these rocks have a similar history to the high-grade metamorphic rocks in the north of the country or not. Petrological investigations combined with geochronological studies were carried out on two gneisses in this area Haad Nai Phlao gneiss are first and khao dating Laem Thong Yang gneissto further understand the timing, metamorphic conditions and tectonic evolution of Peninsular Thailand. These gneisses mainly consist out of feldspar, quartz and two micas. Garnet and aluminosilicate which were described by Kosuwan could not be found. In addition Al-in-hornblende barometry 6. Results from this study suggest that the amphibolebearing gneiss might be derived from the Khao Dat Fa gneiss and that the Haad Nai Phlao gneiss might be the result of contact metamorphism caused by the intrusion of the Khao Pret granite. Similar ages obtained from other metamorphic basement rocks in Thailand e. Doi Inthanon metamorphic core complex suggest that they are all part of the same tectonic entity Sibumasu and therefore share a similar tectonometamorphic history. Schlagwörter Schlagwörter Deutsch. Khanom metamorpher Komplex Thermobarometrie Monazit CHIME Datierung Zirkon SIMS Datierung Thailand. Haupttitel Englisch. Hauptuntertitel Englisch. Paralleltitel Deutsch. Petrogenese von triasischen und kreidezeitlichen metamorphen Gesteinen aus Khanom Halbinsel Thailand. Paralleluntertitel Deutsch. Thermobarometrie, Monazit CHIME und Zirkon SIMS Datierung. AC Nummer.
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