首页> 外文期刊>Neues Jahrbuch fur Mineralogie, Abhandlungen >Isolated alkaline basalt occurrences in the northern Spessart, Germany: Outposts of the Early Miocene Vogelsberg shield volcano?
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Isolated alkaline basalt occurrences in the northern Spessart, Germany: Outposts of the Early Miocene Vogelsberg shield volcano?

机译:孤立的碱性玄武岩在北部斯凯斯特,德国:早期内科斯堡盾牌火山的前哨?

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Four isolated occurrences of Tertiary volcanic rocks in the northern Spessart at Beilstein, Hoher Berg, Madstein and Kasselgrund are relics of volcanic vents or dikes. They display alkaline basalts (s.l.) with mainly trachybasaltic composition, which, from nonnative mineral contents, may be designated as nepheline-bearing alkali-olivine basalts and basanites. In part, centimetre-sized xenoliths of spinel lherzolite occur. According to Ar-Ar dating, the alkaline basalts (s.l.) from Kasselgrund have erupted at 18.1 +/- 0.3 or 19.3 +/- 0.4 Ma, those of Hoher Berg between c. 18 and c. 21 Ma. These ages correspond to the Vogelsberg eruption stage I.A slightly younger Ar-Ar age of 16.8 +/- 0.3 Ma was recorded for the Beilstein basalt, which is in chronological accordance to the turn of Vogelsberg eruption stages II and III. Samples of all four occurrences reveal major and trace element compositions, which are different from those of the Vogelsberg basalts. Compositions of basalts of the stage III from Vogelsberg coincide most with the Spessart basalts. This signals a special position of the northern Spessart volcanic rocks either as a discrete spatial part of the Vogelsberg volcanic suite or as smaller, independent eruption centres.
机译:北方北部山地山脉北部的四个孤立出现,Hoher Berg,Madstein和Kasselgrund是火山口或堤坝的遗物。它们以主要的矿物质含量显示碱性碱基(S.1.),从非矿物质含量,可指定为肾内碱 - 橄榄石基础和基础岩。部分地,发生厘米尺寸的尖晶石XenoLiths。根据Ar-AR的约会,来自卡司格德的碱性玄武岩(S.L.)爆发了18.1 +/- 0.3或19.3 +/- 0.4 mA,Cher Berg之间的HOHER Berg。 18和c。 21 ma。这些年龄对应于vogelsberg喷发阶段I.A为贝尔斯坦玄武岩略有16.8 +/- 0.3 mA的AR-AR Age,这是按时间顺序调节vogelsberg喷发阶段II和III的转弯。所有四种发生的样品都显示出与vogelsberg沼气不同的主要和痕量元素组合物。来自Vogelsberg的第III阶段底座的构成与Spessart BaSalts相一致。这表示北方南部的北方山雀岩石的特殊位置是Vogelsberg火山套件的离散空间部分或作为更小的独立喷发中心。

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