Grundriß der allgemeinen Volkswirtschaftslehre: Verkehr, Handel und Geldwesen. Wert und Preis. Kapital und Arbeit. Einkommen. Krisen, Klassenkämpfe, Handelspolitik. Historische Gesamtentwickelung

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Identifikator:: 1887156356

Document type:: Multivolume work

Author:: Schmoller, Gustav von http://d-nb.info/gnd/118609378

Title:: Grundriß der allgemeinen Volkswirtschaftslehre

Place of publication:: Berlin [u.a.]

Publisher:: Duncker & Humblot

Year of publication:: 1900-

Collection:: Economics Books

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Identifikator:: 1887256288

URN:: urn:nbn:de:zbw-retromon-242253

Document type:: Volume

Author:: Schmoller, Gustav von http://d-nb.info/gnd/118609378

Title:: Verkehr, Handel und Geldwesen. Wert und Preis. Kapital und Arbeit. Einkommen. Krisen, Klassenkämpfe, Handelspolitik. Historische Gesamtentwickelung

Volume count:: 2.1904

Place of publication:: Berlin [u.a.]

Publisher:: Duncker & Humblot

Year of publication:: 1904

Scope:: X, 719 S.

Digitisation:: 2022

Collection:: Economics Books

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Document type:: Multivolume work

Structure type:: Chapter

Title:: Drittes Buch. Der gesellschaftliche Prozeß des Güterumlaufes und der Einkommensverteilung

Collection:: Economics Books

122 ECONOMIC GEOLOGY through the osefi Shaft, which showed a thrust plane by which Paleozoic and Lower Triassic rocks have been pushed on to the Middle Trias. The overthrust bed is nearly half a mile wide, and must have been moved for more than that distance. DBr re DBr ent IAT Eocene- Fiv-~- (¢ Upper Trias - St.Cassian Beds ERE t & DBr Sa Mid Trias {Dolomite & dolomitic Breccia) Muschelkalk DBr DBn Ee, C - Rudi I fas Low Trias - Werfen Bed retaceous - Rudistenkal UpperJrias Wengen Beds Car oe as v nt 3 2s Fie. 37.—THue Ipria MERCURY Mings. Geological map of the district around the Idria Mercury Mines (after Kossmat) ; ee, Eocene-Flysch ; cc, Cretaceous- Rudistenkalk ; t3 t3 Upper Trias-St, Cassian Beds : Upper Trias-Wengen Beds; Dbr., Mid. Trias (Dolomite and Dolomitic Breccia) Muschalkalk ; dotted, Low. Trias-Werfen Beds and Carboniferous-Gailthal Beds; . , | Faults. Lipold’s work has been in general confirmed by the later accounts of the Idria field by Kossmat (tbid., xlix, 1899, pp. 259-96). The rocks belong to the Carboniferous, Trias, Cretaceous, and Eocene Systems. In the Josefi Shaft the

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