Zobrazeno 1 - 9
of 9
pro vyhledávání: '"R. T. Buffler"'
Autor:
R. T. Buffler
Publikováno v:
AAPG Bulletin. 81
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4cbd9bae69193f34e31ea63574ddd4e
https://doi.org/10.1306/3b05c186-172a-11d7-8645000102c1865d
https://doi.org/10.1306/3b05c186-172a-11d7-8645000102c1865d
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 294:137-155
Lowstands of sea level produce significant unconformities, both on the continental shelves as subaerial unconformities and on the ocean basin slopes and floors by submarine erosion and shifts in depositions patterns. This report utilizes seismic data
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78d99a01a5b654c59eeafbc2d7dba626
https://doi.org/10.1098/rsta.1980.0021
https://doi.org/10.1098/rsta.1980.0021
Autor:
V. Kolla, R. T. Buffler
Publikováno v:
Geo-Marine Letters. 3:85-91
The Magdalena Fan can be divided into: upper fan—1:60–1:110 gradients, channels with well-developed levees, generally several subbottom reflectors on 3.5-kHz records, and fine-grained sediments; middle fan—1:110–1:200 gradients, channels with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6407f7fcd8fd34f1d052b5f3366225e1
https://doi.org/10.1007/bf02462452
https://doi.org/10.1007/bf02462452
Publikováno v:
AAPG Bulletin. 60
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75127f48c77b2adb9cd887aa17bb6547
https://doi.org/10.1306/83d92721-16c7-11d7-8645000102c1865d
https://doi.org/10.1306/83d92721-16c7-11d7-8645000102c1865d
Publikováno v:
AAPG Bulletin. 65
Results from 12 reversed refraction profiles each 110 km long have been combined with multichannel reflection data to produce a series of crustal structure sections across the Gulf of Mexico. The refraction data were collected using ocean bottom seis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::293384c202d2cc7d3901257801490009
https://doi.org/10.1306/03b5948b-16d1-11d7-8645000102c1865d
https://doi.org/10.1306/03b5948b-16d1-11d7-8645000102c1865d
Autor:
V. Kolla, R. T. Buffler
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461295709
The Magdalena Fan can be divided into: upper fan—1:60–1:110 gradients, channels with well-developed levees, generally several subbottom reflectors on 3.5-kHz records, and fine-grained sediments; middle fan—1:110–1:200 gradients, channels with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e123d43b56a9a95c738f7778a11554c
https://doi.org/10.1007/978-1-4612-5114-9_12
https://doi.org/10.1007/978-1-4612-5114-9_12
