AND EASTERN ONTARIO. A comparison of the geology of the New Jersey Highlands with that of the Adirondacks and Eastern Ontario reveals the fact that the Franklin formation and the Byram, Losee, and Pochuck gneisses have their equivalents in the northern... Final Report - Seite 128von New Jersey Geological Survey, New Jersey. State Geologist - 1910Vollansicht - Über dieses Buch
| Thomas Chrowder Chamberlin - 1907 - 1104 Seiten
...fragmental volcanic material. The remarkable fact is that all these processes produce amphibolites which cannot be distinguished from one another either by appearance or by chemical analysis. The discovery of their genetic relations affords the key to the solution of some of the most... | |
| University of Illinois (Urbana-Champaign campus) - 1908 - 658 Seiten
...gneiss in New Jersey. In Ontario there is in addition a series of amphibolites which have a three fold origin. Certain ones are considered to represent limestones...geological conditions are thus practically the same in the Adirondacks, Eastern Ontario, and the New Jersey Highlands, except that in the southern area no gabbros... | |
| New Jersey Geological Survey, New Jersey. State Geologist - 1910 - 614 Seiten
...in the banding, of the gneisses and in the ore bodies in the mines. These displacements are nearly always to the right as one faces the fault plane and...area no gabbros occur. In the northern regions the fragmental rocks and the schists derived from them were collectively termed the Grenville series until... | |
| William Shirley Bayley - 1910 - 570 Seiten
...they often seriously affect mining operations in the magnetite mines. ( See also pages I40-J44.) ' COMPARISON OF THE NEW JERSEY HIGHLANDS GEOLOGY WITH...area no gabbros occur. In the northern regions the fragmental rocks and the schists derived from them were collectively termed the Grenville series until... | |
| New Jersey Geological Survey, Geological Survey of New Jersey - 1910 - 568 Seiten
...See also pages 140-144.) COMPARISON OF THE NEW JERSEY HIGHLANDS GEOLOGY WITH THAT OF THE ADIRONDACKS AND EASTERN ONTARIO. A comparison of the geology of...area no gabbros occur. In the northern regions the fragmental focks and the schists derived from them were collectively termed the Grenville series until... | |
| Thomas Chrowder Chamberlin - 1907 - 886 Seiten
...fragmental volcanic material. The remarkable fact is that all these processes produce amphibolites which cannot be distinguished from one another either by appearance or by chemical analysis. The discovery of their genetic relations affords the key to the solution of some of the most... | |
| |