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 163
... anticlinal rather than dome - like . Anticlines and synclines associated with a single dome were found to be overturned in different directions and this leads to a complicated problem as to the type of deformation which produced such ...
... anticlinal rather than dome - like . Anticlines and synclines associated with a single dome were found to be overturned in different directions and this leads to a complicated problem as to the type of deformation which produced such ...
Seite 167
... anticlinal structure , extending from Mayfield southward to Highland and thence southeastward through Dorseys Run to ... anticlines . This overturning is more pro- nounced in the Mayfield - Highland anticline where very gentle dips are ...
... anticlinal structure , extending from Mayfield southward to Highland and thence southeastward through Dorseys Run to ... anticlines . This overturning is more pro- nounced in the Mayfield - Highland anticline where very gentle dips are ...
Seite 183
... anticline . THRUSTING The cross sections and maps ( Plates XXVIII - XXXII ) show clearly that thrusting occurs in many parts of the region , especially in closely folded anticlines and synclines . Minor thrusts may account for relations ...
... anticline . THRUSTING The cross sections and maps ( Plates XXVIII - XXXII ) show clearly that thrusting occurs in many parts of the region , especially in closely folded anticlines and synclines . Minor thrusts may account for relations ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
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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 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