Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)

Paper No. 4
Presentation Time: 1:00 PM-5:00 PM

THE LOWER SILURIAN CLEAR SPRINGS VOLCANIC SUITE: SWORD MOUNTAIN OLIVINE MELILITITE (433+/-3 MA) AND HANGING ROCK DIATREME, WASHINGTON COUNTY, MARYLAND


SMITH II, Robert C., Pennsylvania Geol Survey, 3240 Schoolhouse Road, Middletown, PA 17057, FOLAND, Kenneth A., Department of Geological Sciences, Ohio State Univ, 125 South Oval Mall, Columbus, OH 43210 and NICKELSEN, Richard P., 432 Pheasant Ridge Rd, Lewisburg, PA 17837-8870, roberts@state.pa.us

     The Sword Mountain Olivine Melilitite (OM) on Sword Mountain, previously mapped as a Triassic dike, is locally overlain by a lithified saprolite derived therefrom.  Polished slabs of samples of the OM itself suggest welded lapilli tuff.  A smectite-rich tuff occurs in an ~ 1-ha perched wetland along strike to the north.

     Field mapping indicates that the OM is ~100 m thick, 2.1 km long, and stratabound between the main portion of the Silurian Tuscarora Formation above and the Hanging Rock Diatreme beneath.  The diatreme is variably diluted by Tuscarora sand and is underlain by the thin, lower selvage of the Tuscarora.  The Ordovician Juniata Formation is present beneath the Tuscarora from Pennsylvania southward until it thins just as thin volcaniclastics, tuff, and the OM are progressively approached.  This thinning and eventual absence near the OM may be the result of non-deposition associated with volcanic doming.

     The implied Lower Silurian age was confirmed with detailed incremental-heating 39Ar/40Ar measurements on OM fine-grained groundmass phlogopite (median 2.8% TiO2, 3.6% BaO, and 6.8% F) which yielded concordant spectra with plateaus at 432.6 ± 1.1 Ma.  Rb-Sr analyses of the groundmass phlogopite and whole rock aliquots yield an indistinguishable, concordant age of 434 ± 3 Ma.  For the OM whole rock, calculated initial ratios for 87Sr/86Sr of 0.70370 and 143Nd/144Nd of 0.51233, or eNd[433 Ma]=5.0, indicate a mantle origin with not more than minor crustal interaction.  The OM gives a model TNd age of 0.73 Ga consistent with a depleted mantle source.

     Based on the presence of OM itself and its composition, a continental, initial rifting environment that may have much to do with the development of the Appalachian Basin is suggested.  Although not studied herein, the Beemerville, New Jersey, nepheline syenite beneath the Lower Silurian Shawangunk Formation appears to be related.