Joint 60th Annual Northeastern/59th Annual North-Central Section Meeting - 2025

Paper No. 12-7
Presentation Time: 8:30 AM-5:30 PM

NEW GEOCHRONOLOGICAL AND GEOCHEMICAL CONSTRAINTS ON MAGMATISM IN MIDDLESEX FELLS AREA, SE NEW ENGLAND


TORAMAN, Erkan, Department of Geological Sciences, Salem State University, 352 Lafayette Street, Salem, MA 01970 and RIDGE, John C., Earth and Climate Sciences, Tufts University, Lane Hall 003, Earth and Ocean Sciences, 2 North Hill Rd., Tufts University, Medford, MA, MA 02155

In southeastern New England, a series of Neoproterozoic plutonic, subvolcanic, and volcanic units occur in the Avalon Terrane. While earlier researchers grouped these igneous bodies based on regional correlations, recent studies, particularly those employing high-precision dating methods, have identified significant petrological, compositional and temporal variations within these units. We present new field mapping (Ridge, 2024) along with CA-ID-TIMS U-Pb zircon ages and whole-rock geochemical data from the Middlesex Fells area, offering a more detailed characterization and distinction of rocks that were previously mapped as part of the Dedham Granodiorite and Lynn Volcanics. The Spot Pond Granodiorite yields zircon ages of 609.08±0.24 and 609.11+0.22 Ma, linking it to the Dedham Granodiorite. New mapping documents that the Lynn Volcanic Complex in this region consists of a range of volcanic and subvolcanic units. The Boojum Rock Tuff Member, a dacitic tuff, has an age of 596.35±0.21 Ma, while a rhyolitic flow from the Straw Point area in Stoneham yields an age of 595.27±0.34 Ma. Subvolcanic plutonic units previously lumped with the Dedham now appear to be related to the Lynn. The granitic Lawrence Woods Granophyre displays two age populations of 598.13±0.27 Ma and 596.77±0.54 to 596.50+0.53 Ma while the tonalitic Rams Head Porphyry yields an age of 596.24±0.21 Ma. In the northern Fells and areas further north and northeast the Stoneham Granodiorite has an age of 595.14+0.17. Major element geochemistry displays a calc-alkaline trend, while trace element patterns reveal enrichment of Large Ion-Lithophile Elements (such as K and Rb) and depletion of High Field Strength Elements (such as Ti, P, and Ta), collectively suggesting a subduction zone environment.

Ridge, J.C., 2024, Bedrock Geology of the Middlesex Fells Reservation and Adjoining Parks and Preserves in Malden, Medford, Melrose, Stoneham, and Winchester in Middlesex County, Massachusetts, USA: Map and Explanation, 245 p., 1:4600 scale map (last update February 21, 2024). http://sites.tufts.edu/fellsgeology/