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 43
... planar flow structures Linear and planar flow structures may occur combined . The planes will then eliminate all other planar directions and the linear orientations within the plane will confine all the directions within the planes to ...
... planar flow structures Linear and planar flow structures may occur combined . The planes will then eliminate all other planar directions and the linear orientations within the plane will confine all the directions within the planes to ...
Seite 133
... PLANAR FLOW STRUCTURES Planar flow structure is present in all types of granodiorite in the area . It is characterized by the mutual parallel planar arrangements of minerals , mineral groups , inclusions , groups of inclusions and ...
... PLANAR FLOW STRUCTURES Planar flow structure is present in all types of granodiorite in the area . It is characterized by the mutual parallel planar arrangements of minerals , mineral groups , inclusions , groups of inclusions and ...
Seite 134
... planar minerals are arranged parallel to the plane of flow . Both take the posi- tion of least resistance . The ... planar element , provided , of course , that linear elements are not horizontal . In this case the linear is stronger ...
... planar minerals are arranged parallel to the plane of flow . Both take the posi- tion of least resistance . The ... planar element , provided , of course , that linear elements are not horizontal . In this case the linear is stronger ...
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