%0 Conference Proceedings %B Abstracts with Programs - Geological Society of America %D 2010 %T Arsenic in central Massachusetts bedrock and groundwater %A McTigue, David F. %A Stein, Carol L. %A Brandon, William C. %A Joseph P Kopera %A Keskula, Anna J. %A Koteas, G. Christopher %K #StaffPubs %K alteration %K arsenic %K arsenides %K arsenopyrite %K Ayer Granodiorite %K BEDROCK %K central Massachusetts %K chelmsford granite %K Devonian %K dilation %K discharge %K dissolved materials %K drinking water %K Eh %K fractures %K General geochemistry 02A %K geochemistry %K granites %K ground water %K igneous rocks %K joints %K massachusetts %K metals %K metamorphism %K meteoric water %K overburden %K Paleozoic %K petrography %K plutonic rocks %K pollutants %K reduction %K solubility %K solution %K sulfides %K theoretical models %K United States %X Across the New England "arsenic belt," groundwater arsenic (As) concentrations often exceed the EPA's 0.01-mg/L drinking water standard. In overburden groundwater at a site within this belt in north-central Massachusetts, As has been reported at levels up to 7.6 mg/L. Bedrock at the site consists of Silurian Central Maine Terrane metasediments intruded by the Devonian Ayer granodiorite and Chelmsford granite. Exchange of hydrothermal fluids between these lithologies during intrusion and later deformation, faulting, and metamorphism resulted in crystallization of arsenic-bearing minerals, including arsenopyrite. Quaternary deglaciation and unloading dilated joint systems in the bedrock, allowing increased exposure of the mineralogy to meteoric water. Several arsenopyrite alteration products (e.g., scorodite), of varying solubilities, precipitated on fracture surfaces and along grain boundaries between major phases. In the emerging conceptual model for this site, groundwater is recharged in bedrock uplands and moves downgradient through the fracture network, becoming increasingly reducing as it moves along a flow path. Arsenic dissolved from arsenopyrite and arsenic-bearing alteration phases in bedrock remains in solution until the groundwater discharges to lowland areas hydraulically downgradient. In these adjacent lowlands, glacial sand and gravel overburden lies above the bedrock. When the reducing water reaches more oxidizing conditions, As-sorbing hydrous ferric oxides (HFO) precipitate out on the aquifer solids, resulting in accumulation of As in the deep overburden aquifer. A large landfill at this site, now closed and capped, imposed reducing conditions, and As is mobilized into groundwater by reductive dissolution of the HFO. The presence of elevated As in groundwater is consistent with arsenic-bearing phases generated in granitoids at depth during regional metamorphism, which were subsequently altered, and are being solubilized at present by the circulation of shallow groundwater through varying redox environments. This scenario is supported by geochemical and petrographic studies of the granitoids and the occurrence of the highest groundwater and soil arsenic concentrations in the adjacent deep overburden. %B Abstracts with Programs - Geological Society of America %I Geological Society of America (GSA) : Boulder, CO, United States %C United States %V 42 %P 216 - 217 %8 2010/11/01/ %@ 00167592 %G eng %U https://gsa.confex.com/gsa/2010AM/finalprogram/abstract_182430.htm %N 55 %! Abstracts with Programs - Geological Society of America %0 Conference Proceedings %B Abstracts with Programs - Geological Society of America %D 2004 %T Fracture characterization of crystalline bedrock for groundwater investigations; an example from the Marlborough Quadrangle, Massachusetts %A Scott A Salamoff %A Stephen B Mabee %A Joseph P Kopera %A Donald U Wise %K #StaffPubs %K aquifers %K Assabet River Fault %K BEDROCK %K characterization %K controls %K crystalline rocks %K fractured materials %K fractures %K geographic information systems %K ground water %K Hydrogeology 21 %K hydrology %K information systems %K joints %K Marlborough Quadrangle %K massachusetts %K Middlesex County Massachusetts %K permeability %K preferential flow %K recharge %K style %K testing %K theoretical models %K United States %X Integration of a wide array of structural data with well-field hydrologic testing is increasingly recognized as a critical step in understanding groundwater flow behavior and recharge in crystalline bedrock aquifers (Lyford et al., 2003, Walsh and Lyford, 2002). The Marlborough Quadrangle, about 40 km west of Boston, was selected as a test case of how a state geological survey can most effectively and efficiently collect and present such data in order to better constrain conceptual models of groundwater flow in general and to be of maximum use for hydrologists and consultants working on specific local problems. In this study, 3200 structural measurements were taken by a two-person team over a nine-week period at 68 stations distributed throughout the quadrangle and keyed into a GIS database. Specialized data sheets allowed efficient recording and digitization of orientations, lengths, spacing and mineralization, and separation of various classes of joints and veins. Fault data also included motion direction and sense. Summary maps in GIS format include standard geologic map bases overlain by typical rose diagrams and stereograms and maps such as fracture domains and trajectories, sheeting distribution, foliation trajectories, bedrock elevations, generalized piezometric surface configuration, and overburden type and thickness with separations into permeability class. Geology of the quadrangle can be separated into three zones: (a) north of the Assabet River Fault (ARF), (b) the area between the ARF and 1.5 km-wide Bloody Bluff Fault Zone (BBFZ), and (c) south of the BBFZ. Generalized foliations in the zones are: (a) 215, 50N, (b) 240, 65N, and (c) 270, 45N. Two pervasive, steeply-dipping (>60 degrees ) fracture sets occur throughout the quadrangle: an older 150 degrees set that includes sulfide-bearing veins and fracture surfaces along the ARF and a 015 degrees set of largely unmineralized common joints, macrojoints (>3 m length) and joint zones (av. 1.2 m width). Sheeting and unloading joints are generally coincident with shallow dipping foliation in (c) but cross-cut foliation in (a) and (b). We believe this approach will provide hydrologists and consultants with basic framework data that will expedite and improve the planning of subsurface investigations, construction activities and groundwater exploration. %B Abstracts with Programs - Geological Society of America %I Geological Society of America (GSA) : Boulder, CO, United States %C United States %V 36 %P 113 - 113 %8 2004/03/01/ %@ 00167592 %G eng %U https://gsa.confex.com/gsa/2004NE/finalprogram/abstract_70321.htm %N 22 %! Abstracts with Programs - Geological Society of America %0 Conference Proceedings %B Abstracts with Programs - Geological Society of America %D 2006 %T Fracture patterns across two terrane boundaries in eastern Massachusetts; implications for regional groundwater flow and recharge %A Stephen B Mabee %A Joseph P Kopera %K #StaffPubs %K Avalon Zone %K BEDROCK %K eastern Massachusetts %K faults %K foliation %K fractures %K ground water %K Hydrogeology 21 %K joints %K massachusetts %K Merrimack Belt %K movement %K observations %K patterns %K properties %K recharge %K shear zones %K style %K terranes %K United States %X The integration of structural data and field-based observations is becoming increasingly critical in understanding groundwater flow behavior and recharge potential. Over the past 3 years, the Office of the Massachusetts State Geologist (OMSG) has collected 8225 fracture measurements from 187 stations across 3 adjacent quadrangles as part of its bedrock geologic mapping program. These data provide a north-south transect across the Nashoba Terrane and its boundaries with the Merrimack Belt and Avalon Terranes in eastern Massachusetts. Areas with similar fracture patterns can be grouped into "hydrostructural domains" with distinct hydrogeologic properties. Within the above transect, hydrostructural domains were observed to closely correspond with bedrock lithology and ductile structure, and therefore, tectonic history. Such domains are commonly bounded by faults or intrusive contacts. Common features observed across all domains include a NE-striking regional foliation with corresponding NW-striking, steeply-dipping cross-joints. Strongly layered metasedimentary and metavolcanic rocks of the Merrimack Belt and the Marlborough Formation in the Nashoba Terrane tend to have the most pervasive and closely-spaced foliation-parallel fractures (FPF). Foliation intensity and FPF generally increases towards shear zones and regional fault systems, especially within granites and gneisses. The moderate to steeply dipping, well-developed FPF in these rocks provides a potentially excellent conduit for vertical recharge and a strong NE-trending regional anistropy that may control groundwater flow. Granitoidal rocks have very consistent NS-EW orthogonal networks of vertical fractures and subhorizontal sheeting joints, providing excellent potential for vertical recharge and near-surface lateral flow. Features such as small brittle faults, fracture zones, fold axes, and fracture sets distinct to each domain may dominate local groundwater flow and recharge. Abstract 116563 modified by 72.70.224.253 on 7-12-2006 %B Abstracts with Programs - Geological Society of America %I Geological Society of America (GSA) : Boulder, CO, United States %C United States %V 38 %P 434 - 434 %8 2006/10/01/ %@ 00167592 %G eng %U https://gsa.confex.com/gsa/2006AM/finalprogram/abstract_116563.htm %N 77 %! Abstracts with Programs - Geological Society of America %0 Conference Proceedings %B Abstracts with Programs - Geological Society of America %D 1989 %T Ground truth? Relationship between lineaments and bedrock fabric %A Stephen B Mabee %A Hardcastle, Kenneth C. %A Donald U Wise %K #StaffPubs %K aerial photography %K BEDROCK %K fabric %K faults %K fractures %K granites %K ground truth %K igneous rocks %K joints %K lineaments %K Maine %K orientation %K pegmatite %K plutonic rocks %K quartz veins %K SLAR %K structural analysis %K Structural geology %K Structural geology 16 %K United States %K veins %B Abstracts with Programs - Geological Society of America %I Geological Society of America (GSA) : Boulder, CO, United States %C United States %V 21 %P A68 - A68 %8 1989/01/01/ %@ 00167592 %G eng %N 66 %! Abstracts with Programs - Geological Society of America %0 Conference Proceedings %B Geological Society of America Abstracts with Programs %D 2008 %T The influence of ductile structure and rheological heterogeneity on brittle structures as exhibited by Avalonian granites in southeastern Massachusetts %A Joseph P Kopera %K #StaffPubs %K acadian %K alleghenian %K avalon %K BEDROCK %K dikes %K foliation %K fracture %K fracture system %K fracture trace %K fractures %K granite %K granites %K Hopkinton %K joints %K l-tectonites %K lineaments %K lineation %K Milford %K Upton %X The orientation and geographic distribution of joints, veins, and brittle faults show a conspicuous correlation with the heterogeneous distribution of foliation and lineation intensity in Neo-Proterozoic granites and their deformed counterparts in southeastern Massachusetts. Field mapping and stereonet analysis of brittle and ductile structural data collected during 1:24,000-scale geologic mapping of the Milford quadrangle yielded the following general observations, which suggest that the ductile deformational history of this region appears to have strongly influenced the later development of brittle structures in the same rocks:
Fracture Characterization Map is included as sheets 2 and 3. Water Resources data included as sheet 4.
GIS and metadata forthcoming
%B Open-File Report %7 OFR-07-01 %I Massachusetts Geological Survey %G eng %21:24000
%0 Map %D 2011 %T Progress map of the preliminary bedrock geologic map of the Billerica quadrangle, Massachusetts %A Matthew A Massey %K #BedrockMaps %K #FractureMaps %K #MGSPub %K Bedford %K Berwick formation %K Billerica %K Billerica Schist %K Boxford formation %K Carlisle %K Chelmsford %K Clinton-Newbury Fault Zone %K Concord %K fracture %K gneiss %K joints %K Lowell %K magnetite %K migmatite %K nashoba %K schist %K Spencer Brook Fault %K tadmuck brook schist %K Tewksbury %X This map also contains brittle fracture data as part of the GIS files. This map is a progress report of bedrock geologic mapping currently underway in the Billerica quadrangle. It is a compilation of ongoing field mapping (Massey, this study) and previously published work in the area (Alvord, 1973, 1975; Jahns et al.1959). The Billerica quadrangle is located approximately 20 miles northwest of Boston along Route 3, just south of Lowell, in northeastern Massachusetts, encompassing the northwestern most Nashoba terrane and it’s boundary with the Merrimack belt (Figure 1). In the Billerica quadrangle, the Merrimack Belt consists of limited exposures of highly strained metasediments, or possibly orthoschist derived from reconstituted igne- ous protolith. The Clinton-Newbury fault zone separates the Merrimack Belt from multiply deformed, polymetamorphic biotite gneisses, migmatites, and amphibolites of the Nashoba terrane. %7 OFR11-03 %I Massachusetts Geological Survey %G eng %2 1:24000 %0 Report %D 1923 %T The commercial granites of New England %A Dale, T. Nelson %K #Bibliography %K #LegacyPublications %K Acton %K Becket %K Braintree %K Brockton %K Cohasset %K Dartmouth %K Fall River %K Fitchburg %K granite %K Groton %K Hingham %K joints %K Leominster %K Lynn %K Lynnfield %K Milford %K Milton %K Monson %K New Bedford %K Northbridge %K Otis %K Peabody %K Pelham %K quarries %K quarry %K Quincy %K Revere %K Rockport %K Stoughton %K Townsend %K Uxbridge %K Westford %K Wrentham %XA report on the commerical granites of New England, their properties (jointing, rift, grain, etc...) and descriptions of active quarries in the towns of Acton, Becket, Braintree, Brockton, Cohasset, Dartmouth, Fall River, Fitchburg, Groton, Hingham, Leominster, Lynn, Lynnfield, Milford, Milton, Monson, New Bedford, Northbridge, Otis, Peabody, Pelham, quarries, quarry, Quincy, Revere, Rockport, Stoughton, Townsend, Uxbridge, Westford, and Wrentham.
KEYWORDS: granite, joint, quarry, quarries