U–Pb ages for late magmatism and regional deformation in the Shebandowan Belt, Superior Province, Canada

Abstract

Five precise U–Pb zircon (and titanite) ages from different lithologic units of the Shebandowan greenstone belt in the western Wawa Subprovince of the Superior Province put tight constraints on the time of late Archean magmatism and of two major deformation events.A porphyry sill from the older supracrustal sequence has an age of 2733 ± 3 Ma. Another porphyritic rock, a trondhjemite occurring as a clast in a conglomerate of the unconformably overlying Timiskaming-type supracrustal sequence, formed 2704 ± 2 Ma ago and defines a maximum age for the deposition of the Timiskaming-type sequence. An alkalic volcanic rock from this sequence has been directly dated at [Formula: see text], in accord with the above constraint and with another probable maximum age of deposition given by the date of 2696 ± 2 Ma for the Shebandowan Lake Pluton. A first deformation event (D1) was related to a predominantly vertical tectonic regime and occurred during or before intrusion of the Shebandowan Lake Pluton at 2696 ± 2 Ma. The second deformation event (D2) was caused by northwesterly-directed compression and occurred after [Formula: see text] ago, the age of the Timiskaming-type volcanic rocks. A minimum age for the D2 deformation event, which also affected the adjacent Quetico metasedimentary belt and was probably related to the development of major transcurrent fault systems throughout the Superior Province, is provided by an age of [Formula: see text] for the undeformed, late-kinematic Burchell Lake Pluton.

Great Lakes tectonic zone in Marquette area, Michigan: Implications for Archean tectonics in north-central United States

“…Foliated tonalite from the northern complex (Hammond, 1978) has a U-Pb zircon age of 2,703±16 Ma (recalculated by Zell E. Peterman), and associated rhyolite has a U-Pb zircon age of 2,780+69 Ma (recalculated by Zell E. Peterman). These ages are consistent with more precise U-Pb ages in the Wawa (Shebandowan) subprovince in adjacent Canada (Corfu and Stott, 1986).…”

“…(fig. 8), Corfu and Stott (1986) found that the D l deformation occurred during or before the intrusion of the Shebandowan Lake pluton at 2,696±2 Ma. Deformation D2 in this area occurred between 2,689+3/-2 Ma and 2,684+6/-3 Ma, similar to the age suggested by Davis and others (1989) for D2 in the Rainy Lake wrench zone.…”

U-Pb evidence for a polyorogenic evolution of the HP-HT units of the NW Iberian Massif

“…The solutions were subsequently evaporated, redissolved in 3.1 N HCl and passed through anion ex change columns in HCl medium to purify U and Pb (zircon and monazite). For titanite and rutile, a proce dure using HCl HBr HN0 3 was used (Corfu and Stott 1986). Pb and U were finally collected together in the bombsjSavillex vials used for dissolution and loaded together on outgassed Re fi laments with H 3 P0 4 and silica geL Isotopic ratios were measured on a Finnigan MAT 262 mass spectrometer using up to four Faraday detectors in multicollection mode.…”

Datações U-Pb convencional versus SHRIMP do Maciço estanífero Santa Bárbara, Suíte Granitos últimos de Rondônia, Brasil

“…Executaram-se as análises U-Pb em zircão e monazita por espectrometria de massa por ionização térmica (TIMS) no CPGeo, conforme os procedimentos de Krogh (1973) e Corfu & Stott (1986), sintetizados em Basei et al (1995).…”