EES Departmental Seminar: The low-pressure metamorphic gradient along Nova Scotia’s South Shore, revisited - Dalhousie University
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Title: The low-pressure metamorphic gradient along Nova Scotia’s South Shore, revisited
Abstract: In southwestern Nova Scotia, the metasedimentary rocks of the Meguma terrane exhibit a low-pressure metamorphic gradient from greenschist facies to migmatite in the Queens, Shelburne, and Yarmouth counties. These rocks were described and studied primarily in the 1980s and 1990s with few subsequent studies, leaving questions unanswered concerning their significance to the geological evolution of the Meguma terrane. Metamorphic grade has been observed to increase with proximity to granitoid plutons in this region, but the relative contributions of regional metamorphism vs. contact metamorphism have not been fully disentangled. My planned research program includes several projects in this area, beginning with migmatite and amphibolite-facies cordierite-bearing metapelites. Although a spatial association between migmatite and the Barrington Passage Pluton has been identified, a temporal link has not been established. We will conduct U-Pb geochronology by thermal ionization mass spectrometry (TIMS) to obtain high precision ages of migmatite leucosome and the Barrington Passage Pluton.
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