Analysis of information sources in references of the Wikipedia article "Alpide belt" in English language version.
Die zweite Aenderung besteht darin, dass nun die Ketten, welche jünger sind als das Ober-Carbon oder Perm, sich räumlich scharf abtrennen. Sie liegen fast ganz innerhalb von Senkungen der Altaiden, umrahmt von Linien, die nicht selten das Streichen der Altaiden durchschneiden. Man kann diese umrahmten Ketten als posthume Altaiden ansehen. Die alpinen Ketten (Alpiden) sind ihr wichtigstes Glied. Die Alpiden besitzen einen tertiären Saum. Im variscischen Aussenrande, z. B. ausserhalb der belgischen Kohlenfelder, sieht man nichts Aehnliches. Ueberhaupt ist jüngere Faltung in den Horsten der europäischen Altaiden nur gar selten und in geringem Maasse sichtbar. Es ist, als wäre der Rahmen erstarrt, und die Faltung vom Ober-Carbon an auf die gesenkten Räume eingeschränkt.[In the next place those chains of the Altaides which are younger than the upper Carboniferous and the Permian are separated sharply in space. They lie almost wholly within subsided areas of the Altaides, framed in by lines which frequently cut across the strike of these mountains. We may regard the chains thus framed in as posthumous Altaides. The Alpine chains (Alpides) are their most important member. The Alpides are bordered by a Tertiary zone. Nothing analogous to this is to be seen in the outer margin of the Variscan arc, i.e. outside the Belgian coal-fields. Indeed the younger folding occurs but seldom in the horsts of the European Altaides, and is then only feebly developed. It is as though the frame had become rigid, and the folding, from the upper Carboniferous onwards, had been confined to the downthrown areas. (translated by Hertha B. C. Sollas, under the direction of W. C. Sollas, 1909)]
Figure 7 shows the present extent of the orogenic system related to the obliteration of Paleo-Tethys as compared with that generated during the closure of Neo-Tethys. I call the former the Cimmerides (Figure 7B, I); the latter I define to constitute the Alpides (Figure 7B, II). The Cimmerides and the Alpides may be defined to form the Tethysides, for they both descended from Tethys s.l. (Figure 7A). The Alpine-Himalayan mountain belt therefore consists of two mutually independent, but largely superimposed orogenic complexes (Figure 7A).
Figure 7 shows the present extent of the orogenic system related to the obliteration of Paleo-Tethys as compared with that generated during the closure of Neo-Tethys. I call the former the Cimmerides (Figure 7B, I); the latter I define to constitute the Alpides (Figure 7B, II). The Cimmerides and the Alpides may be defined to form the Tethysides, for they both descended from Tethys s.l. (Figure 7A). The Alpine-Himalayan mountain belt therefore consists of two mutually independent, but largely superimposed orogenic complexes (Figure 7A).
Die zweite Aenderung besteht darin, dass nun die Ketten, welche jünger sind als das Ober-Carbon oder Perm, sich räumlich scharf abtrennen. Sie liegen fast ganz innerhalb von Senkungen der Altaiden, umrahmt von Linien, die nicht selten das Streichen der Altaiden durchschneiden. Man kann diese umrahmten Ketten als posthume Altaiden ansehen. Die alpinen Ketten (Alpiden) sind ihr wichtigstes Glied. Die Alpiden besitzen einen tertiären Saum. Im variscischen Aussenrande, z. B. ausserhalb der belgischen Kohlenfelder, sieht man nichts Aehnliches. Ueberhaupt ist jüngere Faltung in den Horsten der europäischen Altaiden nur gar selten und in geringem Maasse sichtbar. Es ist, als wäre der Rahmen erstarrt, und die Faltung vom Ober-Carbon an auf die gesenkten Räume eingeschränkt.[In the next place those chains of the Altaides which are younger than the upper Carboniferous and the Permian are separated sharply in space. They lie almost wholly within subsided areas of the Altaides, framed in by lines which frequently cut across the strike of these mountains. We may regard the chains thus framed in as posthumous Altaides. The Alpine chains (Alpides) are their most important member. The Alpides are bordered by a Tertiary zone. Nothing analogous to this is to be seen in the outer margin of the Variscan arc, i.e. outside the Belgian coal-fields. Indeed the younger folding occurs but seldom in the horsts of the European Altaides, and is then only feebly developed. It is as though the frame had become rigid, and the folding, from the upper Carboniferous onwards, had been confined to the downthrown areas. (translated by Hertha B. C. Sollas, under the direction of W. C. Sollas, 1909)]
Figure 7 shows the present extent of the orogenic system related to the obliteration of Paleo-Tethys as compared with that generated during the closure of Neo-Tethys. I call the former the Cimmerides (Figure 7B, I); the latter I define to constitute the Alpides (Figure 7B, II). The Cimmerides and the Alpides may be defined to form the Tethysides, for they both descended from Tethys s.l. (Figure 7A). The Alpine-Himalayan mountain belt therefore consists of two mutually independent, but largely superimposed orogenic complexes (Figure 7A).
Die zweite Aenderung besteht darin, dass nun die Ketten, welche jünger sind als das Ober-Carbon oder Perm, sich räumlich scharf abtrennen. Sie liegen fast ganz innerhalb von Senkungen der Altaiden, umrahmt von Linien, die nicht selten das Streichen der Altaiden durchschneiden. Man kann diese umrahmten Ketten als posthume Altaiden ansehen. Die alpinen Ketten (Alpiden) sind ihr wichtigstes Glied. Die Alpiden besitzen einen tertiären Saum. Im variscischen Aussenrande, z. B. ausserhalb der belgischen Kohlenfelder, sieht man nichts Aehnliches. Ueberhaupt ist jüngere Faltung in den Horsten der europäischen Altaiden nur gar selten und in geringem Maasse sichtbar. Es ist, als wäre der Rahmen erstarrt, und die Faltung vom Ober-Carbon an auf die gesenkten Räume eingeschränkt.[In the next place those chains of the Altaides which are younger than the upper Carboniferous and the Permian are separated sharply in space. They lie almost wholly within subsided areas of the Altaides, framed in by lines which frequently cut across the strike of these mountains. We may regard the chains thus framed in as posthumous Altaides. The Alpine chains (Alpides) are their most important member. The Alpides are bordered by a Tertiary zone. Nothing analogous to this is to be seen in the outer margin of the Variscan arc, i.e. outside the Belgian coal-fields. Indeed the younger folding occurs but seldom in the horsts of the European Altaides, and is then only feebly developed. It is as though the frame had become rigid, and the folding, from the upper Carboniferous onwards, had been confined to the downthrown areas. (translated by Hertha B. C. Sollas, under the direction of W. C. Sollas, 1909)]
Figure 7 shows the present extent of the orogenic system related to the obliteration of Paleo-Tethys as compared with that generated during the closure of Neo-Tethys. I call the former the Cimmerides (Figure 7B, I); the latter I define to constitute the Alpides (Figure 7B, II). The Cimmerides and the Alpides may be defined to form the Tethysides, for they both descended from Tethys s.l. (Figure 7A). The Alpine-Himalayan mountain belt therefore consists of two mutually independent, but largely superimposed orogenic complexes (Figure 7A).
