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Pseudotachylyte increases the post-slip strength of faults
RETRODEFORMATION OF CARBONIFEROUS TRACE FOSSILS FROM THE NARRAGANSETT BASIN, UNITED STATES, USING RAINDROP IMPRINTS AND BEDDING-CLEAVAGE INTERSECTION LINEATION AS STRAIN MARKERS
VARIATION IN WINGLESS INSECT TRACE FOSSILS: INSIGHTS FROM NEOICHNOLOGY AND THE PENNSYLVANIAN OF MASSACHUSSETTS
Avalonian perspectives on Neoproterozoic paleogeography: Evidence from Sm-Nd isotope geochemistry and detrital zircon geochronology in SE New England, USA
Sulfate-reducing ammonium oxidation: A thermodynamically feasible metabolic pathway in subseafloor sediment
Subdecadal to multidecadal cycles of Late Holocene North Atlantic climate variability preserved by estuarine fossil pigments
Continuous resistivity profiling to delineate submarine groundwater discharge—examples and limitations
Testing the Efficiency of a Stormwater Runoff Treatment Structure with Anthropogenic Tracers
Elements : Building a New Bridge
Harnessing the Power of Relational Databases for Managing Subsurface Geotechnical and Geologic Data
Pleistocene hydrogeology of the Atlantic continental shelf, New England
The GPR refraction method
700 yr sedimentary record of intense hurricane landfalls in southern New England
Sediment-induced amplification in the Northeastern United States: A case study in Providence, Rhode Island
Earthquake Recurrence Rates in the Central Atlantic United States
Freshwater bivalves (Unionidae), disequilibrium isotopic fractionation, and temperatures
Fracture Trace Analysis with a Geographic Information System “GIS”
Site Response in Providence, Rhode Island: Constraints from Ambient Noise Measurements
The New Bedford area; A preliminary assessment
The New Bedford area is among the least studied in eastern New England, yet an understanding of its tectonic history is essential to the development of a viable paradigm for the assemblage of Avalonian terranes in New England. We review previous work and present the preliminary results of an ongoing program whose goal is to systematically study the structural, petrographic, and geochemical relations in the New Bedford area of southeastern Massachusetts. The region can be divided into two suites of rocks. Group I includes variably deformed granitoids that bear close resemblance to the Proterozoic- to Devonian-aged granitic basement of the Esmond-Dedham terrane. Of particular interest is a newly recognized unit of slightly deformed ~600-Ma, alkalic granite plus diorite, in which contact relations imply comingling of magmas of contrasting composition. In contrast, Group II consists of alaskitic and banded gneisses and schist that are reminiscent of gneissic rocks in western Rhode Island and adjacent Connecticut. Trace-element analyses for both groups are presented, and form the basis for discussion of their possible correlation with other granitoids in southeastern New England. The dominant structural feature in the New Bedford area is a steeply dipping to vertical, east-west–trending foliation that becomes more pervasively developed to the south. This tectonic fabric is strongly oblique to the northeast-trending schistosity of the southern Narragansett Basin, and geometrically more comparable to the east-northeast–trending folds found in the Carboniferous rocks of the northern Narragansett Basin. At present, the geometric and temporal relations among structural features in the New Bedford area and the adjoining Carboniferous rocks remain unclear. Although several interpretations of the regional setting of the lithologies of the New Bedford area are possible, currently the most plausible considers the lithologies of Group I to be a continuation of the Esmond-Dedham terranes, while Group II may be correlative with either the Hope Valley terrane or the Bass River Complex.