克拉石岩和巴尔干山脉华力西期岩浆活动的年代测定

M. Dyulgerov
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引用次数: 0

摘要

报道了用原位锆石和钛矿LA-ICP-MS分析法测定克拉石和巴尔干山脉华力西期岩浆活动的新年龄。结果证实了推测的岩浆岩的华力西时代。Sedemte Prestola钾质花岗质岩石的钛矿测年显示年龄为308.7±9.1 Ma。希普卡镇西部钾质正长岩的锆石测年给出了355±89 Ma的不太一致的结果。对于Lutskan深成岩体的钾碱性正长岩斑岩,Varisan 206Pb/238U年龄在328–308 Ma区间。Lutskan深成岩体钾质石英二长斑岩的锆石测年显示出重要的继承性,206Pb/238U的单一年龄为316Ma,而钛矿测年的结果范围在350至315Ma之间,确定了301±91Ma的差等时线和5.6的MSWD。来自辉长岩闪长玢岩的锆石,切割了绘制在Terra Wasserburg图上的Lutskan花岗质岩石,产生了312±21 Ma的Variscan年龄和296±4.6 Ma的Concordia年龄。
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Dating of Variscan magmatism in Kraishte and Balkan Mts
New age determinations by in-situ zircon and titanite LA-ICP-MS analysis for Variscan magmatic activity from Kraishte and Balkan Mts. are reported. The results confirm the presumed Variscan age of the magmatic rocks. For the Sedemte Prestola potassic granitoids, titanite dating reveal an age of 308.7±9.1 Ma. The zircon dating of potassic syenites, cropping out west of Shipka town gave less consistent results – 355±89 Ma. For potassic-alkaline syenite porphyries from the Lutskan pluton, Variscan 206Pb/238U ages cluster in 328–308 Ma interval. Zircons dating of potassic quartzdiorite porphyry from the Lutskan pluton display important inheritance with single 206Pb/238U age of 316 Ma, whereas results of titanite dating range between 350 and 315 Ma, defining poor isochrone of 301±91 Ma and MSWD of 5.6. Zircons from gabbro-diorite porphyries, cutting the Lutskan granitoids plotted on Terra-Wasserburg diagram yield Variscan age of 312±21 Ma and Concordia age of 296±4.6 Ma.
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