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Willimantic Connecticut

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Journal Article
Journal: GSA Bulletin
Published: 01 October 1969
GSA Bulletin (1969) 80 (10): 2123-2128.
...PERRY H RAHN Abstract Students used Brunton compasses to measure the angles of repose in fresh sand and gravel talus exposed in artificial pits in a kame terrace near Willimantic, Connecticut. The angle of repose was found to average 33.08°, and is independent of exposure direction or material type...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1979
GSA Bulletin (1979) 90 (1): 117-118.
Series: GSA Special Papers
Published: 01 January 1990
DOI: 10.1130/SPE245-p171
... All rock units, many fabrics, and two major faults mapped in the Hadlyme and Willimantic areas, Connecticut, are identified in a 1.45-km-deep research hole drilled at Moodus, Connecticut. Correlation of surface information and existing shallow drill-core data with the Moodus data was partially...
Journal Article
Published: 01 August 2013
Bulletin of the Seismological Society of America (2013) 103 (4): 2344-2355.
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Journal Article
Journal: GSA Bulletin
Published: 01 January 1972
GSA Bulletin (1972) 83 (1): 59-86.
Journal Article
Published: 01 July 2014
Journal of Foraminiferal Research (2014) 44 (3): 230-254.
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Journal Article
Published: 23 January 2013
Geological Magazine (2013) 150 (4): 626-638.
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Journal Article
Journal: Geology
Published: 01 February 2013
Geology (2013) 41 (2): 271-274.
.... The rocks, which form part of the Acadian (Devonian) metamorphic belt in Connecticut (United States), reached ∼1000 °C and minimum pressures of ∼1 GPa based on Zr-in-rutile thermometry, ternary feldspar compositions, and pseudosection analysis. This is the first regional UHT locality in the United States...
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Journal Article
Published: 17 March 2014
Canadian Journal of Earth Sciences (2014) 51 (5): 485-499.
... Gneiss of central Connecticut, and the Early Devonian Quincy Granite of eastern Massachusetts. The data provide evidence for meteoric water alteration of the Avalonian crustal magma sources. Our search for relatively high δ 18 O zircons identified several plutons containing zircons with values exceeding...
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Journal Article
Published: 01 April 2005
American Mineralogist (2005) 90 (4): 592-606.
... thermometry at 800–825 °C ( Moecher 1999 ) for the Willimantic Dome of central Connecticut. No distinct monazite growth episodes younger than domain 4 are recognized in the Lovewell Mountain samples. The slight elevation of Th/U ratio of zone 4 monazite is consistent with the observation that melt...
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Image
Geological maps and sample locations. ( a ) Schematic geological map of Ava...
Published: 17 March 2014
, Connecticut Valley (– Gaspé) synclinorium (or trough); RH, Rowe-Hawley belt; SF, Shelburne Falls arc; Tac, Taconic allochthons or Klippen. BP, Belchertown pluton; MGC, Massabesic gneiss complex; NPG, Narragansett Pier granite; PD, Pelham dome; WD, Willimantic dome; HVSZ, Hope Valley shear zone. Grevillian
Series: GCSSEPM
Published: 01 December 2015
DOI: 10.5724/gcs.15.34.0215
EISBN: 978-1-944966-00-3
... formation of metamorphic-core complex-like structures, such as the Willimantic dome, Connecticut ( Wintsch et al. , 1992 , 1998 ); to Brittle extension and subsequent formation, around 235 Ma, of the Late Triassic-Early Jurassic rift basins in a wide rift zone, extending from the zone of orogenic...