作者: Nicholas Culshaw , Pradeep Bhatnagar
DOI: 10.1139/E01-029
关键词: Geomorphology 、 Batholith 、 Lineation 、 Nova scotia 、 Shear (geology) 、 Bedding 、 Transect 、 Geochemistry 、 Geology 、 Syncline 、 Devonian
摘要: In southern Nova Scotia, the Devonian South Mountain Batholith was emplaced into metasedimentary rocks of Cambro-Ordovician Meguma Group at ca. 370 Ma. The contact eastern end transects a high angle trace subhorizontal, upright Acadian (mid-late Devonian) folds formed in Group. At two locations, where is well exposed, there are contrasting structures country adjacent to anticlinoria and synclinoria, respectively. Regional affected by ductile deformation abut batholith but undisturbed synclinoria. anticlinorial contacts, bedding youngs towards granite, granite side-down shear resulted belt which transposed new contact-parallel fabric. Deflection linear that were initially horizontal (e.g., intersection lineations) illustrates shear. reorientation ...