Zobrazeno 1 - 10
of 67
pro vyhledávání: '"M. D. Max"'
Autor:
Afonso H. Ribeiro, Rafael S. Rbeiro, S. R. Marcella Martins, Mathias R. Luz, M. D. Max Santos, Joaquim de Mira, Vinicios R. Soares
Publikováno v:
2018 13th IEEE International Conference on Industry Applications (INDUSCON).
Deep Learning is part of a broader family of machine learning methods based on learning data representations that is being widely deployed in autonomous vehicles with the purpose to identify and recognize objects on the environment in surroundings. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b30e74bce9de49cdb28a83c02d4efa6d
https://doi.org/10.1109/induscon.2018.8627071
https://doi.org/10.1109/induscon.2018.8627071
Publikováno v:
Marine and Petroleum Geology. 64:31-42
We have identified and analyzed the affect of newly identified gas plumes in the water column from the Barbados Accretionary Complex. Multibeam echo soundings from cruise AT21-02 acquired using a Kongsberg EM122 system were used to define a region wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52996aa4f37be9f0d7d91db2ced31441
https://doi.org/10.1016/j.marpetgeo.2015.02.008
https://doi.org/10.1016/j.marpetgeo.2015.02.008
Publikováno v:
Scopus-Elsevier
Natural leaks of multiphase hydrocarbons from the seafloor are widespread. Characterizing the temporal and spatial variability of these emissions provides baselines for comparison to the magnitude of anthropogenic leaks. Determining leakage rates wil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2103cc45781063366fd1d8b1fb3d4338
https://doi.org/10.4043/27283-ms
https://doi.org/10.4043/27283-ms
Autor:
M. D. Max, R. P. Riddihough
Publikováno v:
Geological Journal. 11:109-120
On the basis of newly released magnetic data, a major fault feature is traced southwest across the Irish continental shelf; along the northwestern margin of the Slyne-Erris Trough, the northern termination of the Porcupine Seabight, and across the Po
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e44fa936b2aeef093c28ea7c9c883c7c
https://doi.org/10.1002/gj.3350110202
https://doi.org/10.1002/gj.3350110202
Publikováno v:
Geological Journal. 23:249-260
The tectonically isolated Farnacht Formation consists of calc-alkaline dacitic-andesitic lavas of volcanic arc affinity. It is situated immediately to the south of the Clew Bay Fault Zone (western continuation of the Highland Boundary Fault Zone of S
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::786ebd2c9774383a8e918fa5b4683d41
https://doi.org/10.1002/gj.3350230305
https://doi.org/10.1002/gj.3350230305
Autor:
C. B. Long, M. D. Max
Publikováno v:
Geological Journal. 20:341-366
Pre-Caledonian basement is exposed in three areas within the Irish orthotectonic Caledonides: 1. In northwest County Mayo the Erris Complex comprises the Annagh Division, which is largely Grenvillian but includes older gneisses, and the Inishkea Divi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72c0de831f35643209b48fc2967d9fd5
https://doi.org/10.1002/gj.3350200404
https://doi.org/10.1002/gj.3350200404
Publikováno v:
Geological Journal. 17:279-295
A Rb-Sr whole-rock isochron study indicates that the entire Donegal granite suite was emplaced into orthotectonic Caledonian (Dalradian) rocks over a short interval during mid-Silurian to earliest-Devonian times. The Thorr pluton, probably the earlie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::761b363eeae413b12ac6133c17f40963
https://doi.org/10.1002/gj.3350170403
https://doi.org/10.1002/gj.3350170403
Autor:
M. D. Max
Publikováno v:
Geological Journal. 24:1-17
Marine turbidites, tuffs, black mudstones and conglomerates of the Cambro-Ordovician Clew Bay Group, were deposited in the E–W elongate transtensional Clew Bay Graben that is centred on Clew Bay, NW Ireland. The group is characterized by extensive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::120d49bbabbab810077a4851f8465e1b
https://doi.org/10.1002/gj.3350240102
https://doi.org/10.1002/gj.3350240102
Autor:
H. A. Van Lunsen, M. D. Max
Publikováno v:
Geological Journal. 10:35-58
The Cambrian sediments in Howth and Ireland's Eye to the northeast of Dublin have been mapped and the submarine deltaic Censure Group and the overlying Nose of Howth Group, which consists of interbedded turbidites and olistostromes, have been disting
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0aacbabc4b68b084a2493664e01bf624
https://doi.org/10.1002/gj.3350100104
https://doi.org/10.1002/gj.3350100104
Publikováno v:
Geological Journal. 19:389-397
The Lough Talt and Easky adamellites in the north-central Ox Mountains inlier were originally regarded as being nearly synchronous in age of emplacement with the more strongly deformed c. 480 Ma Ox Mountains granodiorite. They are now shown by Rb-Sr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0acd6ea6a5df483fa55b02c5dacdaf5b
https://doi.org/10.1002/gj.3350190406
https://doi.org/10.1002/gj.3350190406