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Original Article |
1 1Centro de Investigaciones Geológicas, Calle 1 No. 644, 1900 La Plata, e-mail: crapela@cig.museo.unlp.edu.ar)
2 2British Antarctic Survey, Cambridge CB3 0ET, UK
3 3Present address: NERC Isotope Geosciences Laboratory, Keyworth, Nottingham NG12 5GG, UK
4 4PRISE, Research School of Earth Sciences, The Australian National University, Mills Road, Canberra, A.C.T. 0200, Australia
5 5Departamento de Geología, Universidad Nacional del Sur, San Juan 670, 8000 Bahía Blanca, Argentina
U–Pb sensitive high-resolution ion microprobe data together with geochemical and Nd isotope analyses obtained in the basement complex of the Sierra de la Ventana Fold Belt indicate that the Early Palaeozoic passive margin history of the basin followed Cambrian magmatism related to rifting in a 600 Ma Neoproterozoic crust. The Cambrian episode started with intrusion of 531 ± 4 and 524 ± 5 Ma A- and I-type granites derived from a dehydrated infracrustal source (
Nd530 –3.1 to –5.9), and culminated with eruption of high-Zr peralkaline spherulitic rhyolites derived from an undepleted lithospheric mantle (509 ± 5 Ma; Nd509 +0.5 to +1.0). These rift-related magmatic rocks were covered by shelf sediments deposited along a once-continuous passive margin, encompassing the Sierra de la Ventana Fold Belt, the Cape Fold Belt, the Falkland/Malvinas microplate and the Ellsworth Mountains block in Antarctica. The Cambrian rifting event defined the outline shape of the southern part of Gondwana, and can be regarded as the initiation of the supercontinent stage, which lasted until Jurassic break-up. The conjugate continental fragments separated from Gondwana during the Cambrian rifting could be the source for microcontinents with c. 1000 Ma basement rocks that collided with the proto-Andean margin during Ordovician–Silurian times.
Key Words: U–Pb SHRIMP • Gondwana • geochronology • granites • rifting
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