Amiya K. Ghosh
Kent State University, Kent, OH
Activity
2010
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MORE EVIDENCE THAT THE BLACK HILLS DOMAIN WAS ORIGINALLY PART OF THE ARCHEAN WYOMING CRATON: OCCURRENCES OF 3.8-2.6 GA DETRITAL ZIRCONS IN 2.5-1.9 GA METASEDIMENTARY ROCKS
24 Structural and Tectonic Evolution of the Proterozoic Trans-Hudson–Archean Wyoming Province BoundaryFriday, 23 April 20108:00 AM - 10:00 AMAlpine Room
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U-PB AGES OF ZIRCON, MONAZITE, AND XENOTIME IN THE HARNEY PEAK GRANITE, BLACK HILLS, SD: IMPLICATIONS FOR THE TIMING AND DURATION OF SYN- TO POST-OROGENIC MAGMATISM
24 Structural and Tectonic Evolution of the Proterozoic Trans-Hudson–Archean Wyoming Province BoundaryFriday, 23 April 20108:00 AM - 10:00 AMAlpine Room