加泰罗尼亚-巴利阿里盆地边缘古磁学结果的综合。

J. Parés, F. Sábat, R. Freeman
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引用次数: 7

摘要

通过对CatalanBalearie海槽(主要是catalancoastal Range和Mallorca)边缘的三叠纪、侏罗纪和第三纪古地磁资料的研究和比较,我们宣布了一些关于它们的地球动力学意义的考虑。从这个意义上说,应该注意到加泰罗尼亚海岸山脉相对于伊比利亚西部的古地磁方向的系统顺时针旋转,同样,马略卡岛相对于加泰罗尼亚方向的方向的顺时针旋转:Institut Jaume Almera, C.S.I.C, Marti Franques sIn, 08028 Barcelo* na(西班牙)。[6]刘建军,刘建军,刘建军,等。构造旋转的历时性也被观察到。对这些结果的详细分析,其中一些仍然是初步的,使我们能够在加泰罗尼亚-巴利里海槽地球动力学演化的相同背景下解释观察到的旋转。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Síntesis de los resultados paleomagnéticos de los bordes de la cuenca Catalano-Balear.
The study and comparison between the Triassic, Jurassic and Tertiary available paleomagnetic data from the emerged margins of the CatalanBalearie Trough (essentially Catalan Coastal Range and Mallorca), lead us to announce some considerations relative to their geodynamic implications. In this sense, it should be noted a systematic clockwise rotation of the paleomagnetic directions from the Catalan Coastal Range relative to those from the western part of Iberia and similarly, a clockwise rotation of the directions from Mallorca relative to those from the Catalan Direccion actual: Institut Jaume Almera, C.S.I.C., Marti i Franques sIn, 08028 Barcelo* na (Spain). 60 J. Al. Pares, R. Freeman y E Sabat margin. A diachrony of the tectonie rotations is also observed. The detailed analysis of these results, some of them still preliminary, allows us to explain the observed rotations within the same context of the geodynamie evolution of the Catalan-Balearie Trough.
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