The Rand Granite in the southern Schwarzwald and its geodynamic significance in the Variscan belt of SW Germany

• Published in: International journal of earth sciences : Geologische Rundschau Vol. 92; no. 6; pp. 821 - 842
• Main Authors: Hann, H. P., Chen, F., Zedler, H., Frisch, W., Loeschke, J.
• Format: Journal Article
• Language: English
• Published: Berlin Springer Nature B.V 01-12-2003
• Subjects: Boundaries; Continental crust; Continental margins; Geology; Granite; High temperature; Metamorphism; Plate tectonics
• ISSN: 1437-3254; 1437-3262
• DOI: 10.1007/s00531-003-0361-8

The Rand Granite is a heterogeneous metamorphosed granitoid rock complex with numerous wallrock inclusions situated in the Moldanubian Zone at the southern margin of the Central Schwarzwald Gneiss Complex. It is a largely mylonitized elongated body and is thrust over the Badenweiler-Lenzkirch Zone forming a nappe with shear zones along its northern and southern boundaries. It comprises meta-granites, meta-trondhjemites and biotite augen gneisses derived from monzogranites to granodiorites. Mineral behaviour indicates that the magmatic body has been deformed under upper greenschist facies conditions. Nappe thrusting, which also affected the South Schwarzwald Gneiss Complex, occurred in Visean time during high-temperature / low-pressure metamorphism. Kinematic indicators in the mylonites document E- to ESE-directed nappe transport, highly transpressive relative to the trend of the nappe boundaries and the foliation. The trondhjemites formed at 351 +5/-4 Ma, predating the Variscan HT metamorphism. They have initial ε^sub Nd^-values of +6.6 to +6.7 and relatively low initial ^sup 87^Sr/^sup 86^Sr ratios (0.7042 to 0.7063), indicating a predominant mantle origin. The granites and protoliths of the biotite augen gneisses probably crystallised between 436 and 377 Ma, suggested by U-Pb zircon model ages. They are different from the trondhjemites with low initial ε^sub Nd^-values (-4.7 to -3.3) and higher initial ^sup 87^Sr/^sup 86^Sr ratios (0.7068-0.7077), indicating that large part of the Rand Granite originated from anatexis of continental crust. Internal structure of zircons from the Rand Granite reveals mixing of magmas derived from both mantle and crust sources. These new data support an interpretation that the Rand Granite developed along an active continental margin and therefore represents a possible root of a Variscan magmatic arc.[PUBLICATION ABSTRACT]