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GEOREF RECORD

Low P-T Caledonian resetting of U-rich Paleoproterozoic zircons, central Sweden

Karin Hogdahl, L. Peter Gromet and Curt Broman
Low P-T Caledonian resetting of U-rich Paleoproterozoic zircons, central Sweden
American Mineralogist (April 2001) 86 (4): 534-546

Abstract

Uranium-rich zircons from a Paleoproterozoic, high-grade deformation zone in the Fennoscandian Shield, central Sweden, show an almost complete resetting of the U-Pb system in early Phanerozoic time. A mylonitic gneiss in the deformation zone contains two types of highly discordant (>70%), U-rich zircons: large, brown, cloudy prisms, and small milky-white irregularly shaped grains. The gneiss also contains mostly clear prismatic zircon of lower U content with mildly discordant to concordant U-Pb ages. Laser Raman spectroscopy reveals that the dark cathodoluminescent areas in brown zircons have a highly metamict crystal structure, whereas the structures of both the dark cathodoluminescent milky-white grains and the bright cathodoluminescent clear prisms have higher degrees of crystallinity. Age dates obtained by U-Pb SIMS analysis of 40 zircons of the three types described above range continuously from concordant at 1871+ or -11 Ma to 98% discordant at 384+ or -15 Ma. The strongly discordant zircons clearly have suffered severe disturbance at about the time of the Caledonian orogeny. However, Caledonian metamorphic temperatures and pressures in this region did not exceed 150-200 degrees C and 1-3 kbar, too low to strongly disturb the U-Pb systematics in non-metamict zircon by thermal means alone. Independent evidence indicates that saline fluids were circulating in the Paleoproterozoic basement rocks at this time, possibly driven by hydrological gradients generated in front of the encroaching Caledonian orogenic wedge. These low-temperature saline fluids are inferred to be responsible for causing both strong Pb loss in the mostly metamict brown zircons via a diffusive process, and the formation of small milky-white zircon via a low-temperature recrystallization or dissolution/re-precipitation process.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 86
Serial Issue: 4
Title: Low P-T Caledonian resetting of U-rich Paleoproterozoic zircons, central Sweden
Affiliation: Swedish Museum of Natural History, Laboratory for Isotope Geology, Sweden
Pages: 534-546
Published: 200104
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 53
Accession Number: 2001-049395
Categories: Geochronology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. geol. sketch maps
N62°57'00" - N62°57'00", E14°45'00" - E14°45'00"
Secondary Affiliation: Brown University, USA, United StatesStockholm University, SWE, Sweden
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2018, American Geosciences Institute.
Update Code: 200115
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