Report, Band 13John Hopkins Press, 1937 CONTENTS.--Vol. I (1897)--Vol. II (1898)--Vol. III (1899)--Vol. IV (1902)--Vol. V (1905)--Vol. VI (1906)--Vol. VII (1908)--Vol. VIII (1909)--Vol. IX (1911)--Vol. X (1918)--Vol. XI (1922)--Vol. XII (1928)--Vol. XIII (1937)--Vol. XIV (1941) |
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Seite 58
... deformation that has taken place and since this deformation is closely related to the temperature and pressure governing the deformation , the folds which result grade as much into each other as the conditions . A strict and schematical ...
... deformation that has taken place and since this deformation is closely related to the temperature and pressure governing the deformation , the folds which result grade as much into each other as the conditions . A strict and schematical ...
Seite 69
... deformation by another cleavage . They can be transected by later cleavage planes at any angle and their intersection can be parallel to the axes of the fold or can deviate from it considerably . Usually this later cleavage is not ...
... deformation by another cleavage . They can be transected by later cleavage planes at any angle and their intersection can be parallel to the axes of the fold or can deviate from it considerably . Usually this later cleavage is not ...
Seite 185
... deformation renders a simple connection between the two units unlikely . The deformation of the Glenarm Series may have affected the Baltimore gneiss complex only to the extent of intensifying the older dome structures . The deformation ...
... deformation renders a simple connection between the two units unlikely . The deformation of the Glenarm Series may have affected the Baltimore gneiss complex only to the extent of intensifying the older dome structures . The deformation ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
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Häufige Begriffe und Wortgruppen
abundant amphibolite amygdules anticlines aplite axes of folding axis Baltimore gabbro Baltimore gneiss banding bedding biotite Bridge Chattolanee dome Chesapeake chlorite cleavage planes Conowingo Dam County Creek cross joints Crosswicks clay crystals deformation Delaware Deposit granodiorite complex diagrams dikes direction east Englishtown Englishtown sand epidote exposures fault feet feldspar flow cleavage flow lines flow structures foliation fossils fracture cleavage gabbro geologic Glenarm Glenarm Series grains granite porphyry granodiorite hornblende igneous rocks inclusions intrusive Jersey lamprophyre linear structures localities marble Marshalltown Marshalltown formation Maryland massive metamorphism metamorphosed mile minerals Mount Laurel Mount Laurel sand northeast occur orientation parallel pegmatite Piedmont planar Plate pluton Port Deposit Port Deposit granodiorite primary quarry quartz diorite quartzite recrystallization region relation schist schistosity sediments Setters formation shear specimen strike Susquehanna River syncline Towson dome transect unconformity Upper Cretaceous volcanics wall rock Wissahickon schist Woodstock dome