Geological Notes On Oil Structures
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In our eReader you can find the full English version of the book. Read Geological Notes On Oil Structures 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 Geological Notes On Oil Structures
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That is a terrace such as is known to oil fields. While it may be true that after passing upward along the inclination of the beds falling away from the terraced area, and across the latter area also, the beds will again disclose the inclination noted further down the dip, and that such inclination will continue to rise until the point of action or the apex of the dip-plane is found. The fact remains that the terrace is present, and that oil will not continue to pass along under a level stratum... or move through one, though it may accumulate in it after it is driven from lower levels in the dip-plane because of the greater specific gravity of water.
DESCRIPTION OF STRUCTURES The Dip-plane Structure is that area of change of degree of inclination of the dipping beds, and may be present at any point along the dip of the strata. Oil will move upward through a porous stratum as water passes to the low levels, but will not have the freedom of action at places where the pitch exhibits any considerable change of degree.
What to read after Geological Notes On Oil Structures?
You can find similar books in the "Read Also" column, or choose other free books by Edward Allison Hill to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
That is a terrace such as is known to oil fields. While it may be true that after passing upward along the inclination of the beds falling away from the terraced area, and across the latter area also, the beds will again disclose the inclination noted further down the dip, and that such inclination will continue to rise until the point of action or the apex of the dip-plane is found. The fact remains that the terrace is present, and that oil will not continue to pass along under a level stratum... or move through one, though it may accumulate in it after it is driven from lower levels in the dip-plane because of the greater specific gravity of water.
DESCRIPTION OF STRUCTURES The Dip-plane Structure is that area of change of degree of inclination of the dipping beds, and may be present at any point along the dip of the strata. Oil will move upward through a porous stratum as water passes to the low levels, but will not have the freedom of action at places where the pitch exhibits any considerable change of degree.
What to read after Geological Notes On Oil Structures?
You can find similar books in the "Read Also" column, or choose other free books by Edward Allison Hill to read onlineMoreLess
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