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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... large experience. That is a degree in the school of Christ that will outweigh all the doctoral degrees of all the universities. We need a larger work, and by this we do not mean we need a larger sphere. What we need is a better quality ...
... large experience. That is a degree in the school of Christ that will outweigh all the doctoral degrees of all the universities. We need a larger work, and by this we do not mean we need a larger sphere. What we need is a better quality ...
Seite 50
... larger chamber , 112 × 84 μ ; of the smaller chamber 70 X 112 μ . The wall between the chambers is slightly curved and is about 10 μ thick ( measurement only approximate ) . Auxiliary chambers , diameter , 84 × 56 μ . The equatorial ...
... larger chamber , 112 × 84 μ ; of the smaller chamber 70 X 112 μ . The wall between the chambers is slightly curved and is about 10 μ thick ( measurement only approximate ) . Auxiliary chambers , diameter , 84 × 56 μ . The equatorial ...
Seite 215
Marcelle K. BouDagher-Fadel. 215. Chapter. 5. The. Mesozoic. larger. benthic. foraminifera: the. Cretaceous. 5.1. Introduction Although more than a third of the larger benthic foraminifera became extinct towards the end of the Tithonian, ...
Marcelle K. BouDagher-Fadel. 215. Chapter. 5. The. Mesozoic. larger. benthic. foraminifera: the. Cretaceous. 5.1. Introduction Although more than a third of the larger benthic foraminifera became extinct towards the end of the Tithonian, ...
Inhalt
Page | 19 |
Preface | 25 |
Primary Elements in Igneous Rocks of the Piedmont | 37 |
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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