TY - JOUR

T1 - Exceptional preservation of reidite in the Rochechouart impact structure, France

T2 - New insights into shock deformation and phase transition of zircon

AU - Plan, Anders

AU - Kenny, Gavin G.

AU - Erickson, Timmons M.

AU - Lindgren, Paula

AU - Alwmark, Carl

AU - Holm-Alwmark, Sanna

AU - Lambert, Philippe

AU - Schersten, Anders

AU - Soderlund, Ulf

PY - 2021/8/19

Y1 - 2021/8/19

N2 - Reidite, the high-pressure zircon (ZrSiO4) polymorph, is a diagnostic indicator of impact events. Natural records of reidite are, however, scarce, occurring mainly as micrometer-sized lamellae, granules, and dendrites. Here, we present a unique sequence of shocked zircon grains found within a clast from the Chassenon suevitic breccia (shock stage III) from the similar to 200 Ma, 20-50 km wide Rochechouart impact structure in France. Our study comprises detailed characterization with scanning electron microscopy coupled with electron backscatter diffraction with the goal of investigating the stability and response of ZrSiO4 under extreme P-T conditions. The shocked zircon grains have preserved various amounts of reidite ranging from 4% up to complete conversion. The grains contain various variants of reidite, including the common habits: lamellae and granular reidite. In addition, three novel variants have been identified: blade, wedge, and massive domains. Several of these crosscut and offset each other, revealing that reidite can form at multiple stages during an impact event. Our data provide evidence that reidite can be preserved in impactites to a much greater extent than previously documented. We have further characterized reversion products of reidite in the form of fully recrystallized granular zircon grains and minute domains of granular zircon in reidite-bearing grains that occur in close relationship to reidite. Neoblasts in these grains have a distinct crystallography that is the result of systematic inheritance of reidite. We interpret that the fully granular grains have formed from prolonged exposure of temperatures in excess of 1200 degrees C. Reidite-bearing grains with granular domains might signify swift quenching from temperatures close to 1200 degrees C. Grains subjected to these specific conditions therefore underwent partial zircon-to-reidite reversion, instead of full grain recrystallization. Based on our ZrSiO4 microstructural constraints, we decipher the grains evolution at specific P-T conditions related to different impact stages, offering further understanding of the behavior of ZrSiO4 during shock.

AB - Reidite, the high-pressure zircon (ZrSiO4) polymorph, is a diagnostic indicator of impact events. Natural records of reidite are, however, scarce, occurring mainly as micrometer-sized lamellae, granules, and dendrites. Here, we present a unique sequence of shocked zircon grains found within a clast from the Chassenon suevitic breccia (shock stage III) from the similar to 200 Ma, 20-50 km wide Rochechouart impact structure in France. Our study comprises detailed characterization with scanning electron microscopy coupled with electron backscatter diffraction with the goal of investigating the stability and response of ZrSiO4 under extreme P-T conditions. The shocked zircon grains have preserved various amounts of reidite ranging from 4% up to complete conversion. The grains contain various variants of reidite, including the common habits: lamellae and granular reidite. In addition, three novel variants have been identified: blade, wedge, and massive domains. Several of these crosscut and offset each other, revealing that reidite can form at multiple stages during an impact event. Our data provide evidence that reidite can be preserved in impactites to a much greater extent than previously documented. We have further characterized reversion products of reidite in the form of fully recrystallized granular zircon grains and minute domains of granular zircon in reidite-bearing grains that occur in close relationship to reidite. Neoblasts in these grains have a distinct crystallography that is the result of systematic inheritance of reidite. We interpret that the fully granular grains have formed from prolonged exposure of temperatures in excess of 1200 degrees C. Reidite-bearing grains with granular domains might signify swift quenching from temperatures close to 1200 degrees C. Grains subjected to these specific conditions therefore underwent partial zircon-to-reidite reversion, instead of full grain recrystallization. Based on our ZrSiO4 microstructural constraints, we decipher the grains evolution at specific P-T conditions related to different impact stages, offering further understanding of the behavior of ZrSiO4 during shock.

KW - HIGH-PRESSURE

KW - U-PB

KW - RADIATION-DAMAGE

KW - VREDEFORT IMPACT

KW - ZRSIO4

KW - METAMORPHISM

KW - CRYSTALLINE

KW - TEMPERATURE

KW - QUARTZ

KW - CRATER

U2 - 10.1111/maps.13723

DO - 10.1111/maps.13723

M3 - Journal article

VL - 56

SP - 1795

EP - 1828

JO - Meteoritics and Planetary Science

JF - Meteoritics and Planetary Science

SN - 1086-9379

IS - 10

ER -