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) |
Im Buch
Ergebnisse 1-3 von 74
Seite 166
... strike parallel to the longest axis of the uplift , circular in which the ele- ments parallel the flanks of round domes , and transgressing , the strike of the axes of folding and linear parallelism transgresses the axis of uplift and ...
... strike parallel to the longest axis of the uplift , circular in which the ele- ments parallel the flanks of round domes , and transgressing , the strike of the axes of folding and linear parallelism transgresses the axis of uplift and ...
Seite 170
... strike . The direction was generalized in many places , because of local irregularities in the strike of linear elements . The general interdependence can very well be observed in the distinct change in direction of the cross joints ...
... strike . The direction was generalized in many places , because of local irregularities in the strike of linear elements . The general interdependence can very well be observed in the distinct change in direction of the cross joints ...
Seite 209
... strike joint faces , there is in places a second weaker direction of slickensiding which shows nearly horizontal movement . This is later than the regional tension joints and offsets them to a considerable extent . In one locality the ...
... strike joint faces , there is in places a second weaker direction of slickensiding which shows nearly horizontal movement . This is later than the regional tension joints and offsets them to a considerable extent . In one locality the ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
11 weitere Abschnitte werden nicht angezeigt.
Andere Ausgaben - Alle anzeigen
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