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 157
... Setters formation . Marble accompanies the northern border of the Towson dome from Greenwood along the southeastern flank , where it is apparently thrust out , to Hollins Station along the western end where it is cut out by a fault ...
... Setters formation . Marble accompanies the northern border of the Towson dome from Greenwood along the southeastern flank , where it is apparently thrust out , to Hollins Station along the western end where it is cut out by a fault ...
Seite 165
... Setters formation followed this surface closely and is comparatively free from minor folds . On the other hand , the sediments ( marble and schist ) above the Setters formation are tightly folded and , as a rule , not closely related to ...
... Setters formation followed this surface closely and is comparatively free from minor folds . On the other hand , the sediments ( marble and schist ) above the Setters formation are tightly folded and , as a rule , not closely related to ...
Seite 185
... Setters formation seems closely attached , is of very much larger order of magnitude than minor folding in the gneiss complex below or in the marble and schist above . Major folds are overturned toward the north as well as to the south ...
... Setters formation seems closely attached , is of very much larger order of magnitude than minor folding in the gneiss complex below or in the marble and schist above . Major folds are overturned toward the north as well as to the south ...
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