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 45
Seite 69
... 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 accompanied by as extensive a recrystallization as the earlier ...
... 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 accompanied by as extensive a recrystallization as the earlier ...
Seite 204
... later schistosity . The shape of both amygdules and inclu- sions is , as a rule , lenticular but without an excessive length - width ratio ; an indication that flow was not strong in the primary lava . There has been little stretching ...
... later schistosity . The shape of both amygdules and inclu- sions is , as a rule , lenticular but without an excessive length - width ratio ; an indication that flow was not strong in the primary lava . There has been little stretching ...
Seite 236
... later granite ( Ellicott City granite ) . All later deformation could only serve to modify its primary outlines slightly and to produce secondary structures which now predominate and have to a large extent obliterated the earlier ones ...
... later granite ( Ellicott City granite ) . All later deformation could only serve to modify its primary outlines slightly and to produce secondary structures which now predominate and have to a large extent obliterated the earlier ones ...
Inhalt
Preface | 25 |
Economic Significance of Detailed Structural Investigations | 31 |
Structures in Igneous Rocks | 36 |
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 canal 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 volcanics wall rock Wissahickon schist Woodstock dome