Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Nat G. Smith"'
Publikováno v:
The Leading Edge. 34:1332-1338
During the last two decades, several studies have shown that organic-rich shales are characterized by strong velocity anisotropy. It is well known that these types of rocks exhibit strong polar anisotropy, also known as vertical transverse isotropy (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ea6aa444f2e9f975ad33c98ece79ac5
https://doi.org/10.1190/tle34111332.1
https://doi.org/10.1190/tle34111332.1
Publikováno v:
The Leading Edge. 15:261-266
In the April 1996 “Interpreter’s Corner,” Figure 8 erroneously duplicated another figure. Instead, it should have contained the map featured below. In addition, the line directions were accidentally cropped. Please note that the line directions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5065c6228f698fe9f4ce1c172dbcc5ad
https://doi.org/10.1190/1.1437304
https://doi.org/10.1190/1.1437304
Autor:
Allen J. Bertagne, Nat G. Smith
Publikováno v:
AAPG Bulletin. 79
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e0dd498481cf9d06e5139cdd5e2ac68
https://doi.org/10.1306/8d2b1dd6-171e-11d7-8645000102c1865d
https://doi.org/10.1306/8d2b1dd6-171e-11d7-8645000102c1865d
Publikováno v:
The Leading Edge. 15:720-720
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b2a63137c83a30d4cd5c95fcac64bbd
https://doi.org/10.1190/1.1487183
https://doi.org/10.1190/1.1487183