@proceedings {299,
	title = {Ground truth? Relationship between lineaments and bedrock fabric},
	volume = {21},
	year = {1989},
	note = {Accession Number: 1991-043915; Conference Name: Geological Society of America, 1989 annual meeting; St. Louis, MO, United States; Conference Date: 19891106; Language: English; Coden: GAAPBC; Collation: 1; Collation: A68; Publication Types: Abstract Only; Serial; Conference document; Updated Code: 1991; Monograph Title: Geological Society of America, 1989 annual meeting; Monograph Author(s): Dymek, Robert F. [chairperson]; Shelton, Kevin L. [chairperson]; Reviewed Item: Analytic},
	month = {1989/01/01/},
	pages = {A68 - A68},
	publisher = {Geological Society of America (GSA) : Boulder, CO, United States},
	address = {United States},
	keywords = {$\#$StaffPubs, aerial photography, BEDROCK, fabric, faults, fractures, granites, ground truth, igneous rocks, joints, lineaments, Maine, orientation, pegmatite, plutonic rocks, quartz veins, SLAR, structural analysis, Structural geology, Structural geology 16, United States, veins},
	isbn = {00167592},
	author = {Stephen B Mabee and Hardcastle, Kenneth C. and Donald U Wise}
}
@article {305,
	title = {Influence of rock fabric on fracture attribute distribution and implications for groundwater flow in the Nashoba Terrane, eastern Massachusetts},
	journal = {Journal of Structural Geology},
	volume = {30},
	year = {2008},
	note = {Accession Number: 2009-050694; Language: English; Coden: JSGEDY; Collation: 14; Publication Types: Serial; Updated Code: 200928; Reviewed Item: Analytic},
	month = {2008/04/01/},
	pages = {464 - 477},
	publisher = {Elsevier : Oxford, International},
	address = {International},
	abstract = {Attributes (i.e. trace-length, spacing, termination and orientation) of joints and foliation-parallel fractures (FPFs) are used to assess the influence of lithology and fabric on fracture type and distribution in metamorphic and igneous rocks of the Nashoba terrane, Massachusetts. Orientations of NE-SW and NW-SE trending joints are consistent throughout the region, whereas FPFs are sub-parallel to the axis of the terrane. Joint spacing generally decreases to the northeast across the terrane reflecting lithologic changes from metamorphic to igneous rock types. Although trace-length and spacing frequency distributions of both joints and FPFs are best described by lognormal functions, FPFs possess narrower fracture spacing than joints. Median fracture trace-lengths of all FPFs are comparable to those of all steep joints, but the median fracture spacing is half that of all steep joints. Trace-lengths of FPFs vary as a function of the degree of development of foliation. Fracture attributes and groundwater flow models suggest that FPFs may significantly increase fracture connectivity and potential for groundwater recharge. FPFs may account for as much as 30\% of flow in fracture networks suggesting that in addition to joints, FPFs play a significant role in groundwater hydraulics that may include imparting flow anisotropy on the groundwater system.},
	keywords = {$\#$StaffPubs, foliation, fractures, ground water, Hydrogeology 21, joints, massachusetts, movement, Nashoba terrane, preferred orientation, statistical distribution, structural analysis, Structural geology, style, terranes, United States},
	isbn = {01918141},
	url = {http://www.sciencedirect.com/science/article/pii/S0191814107002362},
	author = {Alex K Manda and Stephen B Mabee and Donald U Wise}
}
