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 198
... foliation . The feldspar was determined as oligoclase , about Ab , An . Quartz and feldspar are about equal . The larger feldspar grains , about 1.0 mm . , are granulated and show orientation at small angles to the foliation as if they ...
... foliation . The feldspar was determined as oligoclase , about Ab , An . Quartz and feldspar are about equal . The larger feldspar grains , about 1.0 mm . , are granulated and show orientation at small angles to the foliation as if they ...
Seite 206
... foliation . Inclusions in all the granites parallel the foliation when the shape of the inclusions is elongate or tabular . Equidimensional inclusions show no orientation ( 26 ) . These inclusions are both autoliths and xeno- liths in ...
... foliation . Inclusions in all the granites parallel the foliation when the shape of the inclusions is elongate or tabular . Equidimensional inclusions show no orientation ( 26 ) . These inclusions are both autoliths and xeno- liths in ...
Seite 231
... foliation and fracture cleavage is in part followed by acid veins . Everywhere the trend parallels the contact of the complex with the older rocks , even between Hollofield and Oella where the primary foliation is not always parallel to ...
... foliation and fracture cleavage is in part followed by acid veins . Everywhere the trend parallels the contact of the complex with the older rocks , even between Hollofield and Oella where the primary foliation is not always parallel to ...
Inhalt
The Application of Recent Structural Methods in the Interpretation | 27 |
General Statement | 49 |
Types and Manner of Producing folds | 55 |
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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 microscope 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