Sundry Geological Problems
Sundry Geological Problems
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In our eReader you can find the full English version of the book. Read Sundry Geological Problems Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Sundry Geological Problems
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Similar instances can be had from the hematite deposits in Cumberland, where brachjppodes and corals have been converted into hematite retaining their form. By Konerud- kollen zinc mines near Drammen one finds corals filled with crystals of idocrase. Ore deposits are largely formed by diffusion and migration of igneous emanations of metal- liferous matter having taken place within the sediments adjacent to an eruptive according to laws analogous to those obtaining for the segregation of ores wi...thin eruptives. Thus effects of pressure play a similar role also for ore deposits in sediments. The sediments have been able to get into a state sufficiently fluid to allow of the migration of metalliferous particles, but not sufficiently fluid to obli- terate all the fossils.
The post-silurian eruptives of the Christiania district, geologically speaking, have their porphyric rim and their border sheeting, in red sandstones as at Krokkleven and Holmestrand or in dark hornblendic slate as at Krekling, Eker.
What to read after Sundry Geological Problems?
You can find similar books in the "Read Also" column, or choose other free books by G Gudbrand Henriksen to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Similar instances can be had from the hematite deposits in Cumberland, where brachjppodes and corals have been converted into hematite retaining their form. By Konerud- kollen zinc mines near Drammen one finds corals filled with crystals of idocrase. Ore deposits are largely formed by diffusion and migration of igneous emanations of metal- liferous matter having taken place within the sediments adjacent to an eruptive according to laws analogous to those obtaining for the segregation of ores wi...thin eruptives. Thus effects of pressure play a similar role also for ore deposits in sediments. The sediments have been able to get into a state sufficiently fluid to allow of the migration of metalliferous particles, but not sufficiently fluid to obli- terate all the fossils.
The post-silurian eruptives of the Christiania district, geologically speaking, have their porphyric rim and their border sheeting, in red sandstones as at Krokkleven and Holmestrand or in dark hornblendic slate as at Krekling, Eker.
What to read after Sundry Geological Problems?
You can find similar books in the "Read Also" column, or choose other free books by G Gudbrand Henriksen to read onlineMoreLess
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