Zobrazeno 1 - 10
of 41
pro vyhledávání: '"I. P. MARTINI"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 101, Iss 3 (2017)
Several Upper Tortonian to Lower Messinian sedimentary facies were recognized and mapped in the M.te Soldano area at the southeastern end of the extensional Basin of Volterra in the Nothern Apennines in Tuscany. They consist of (a) disorganized coars
Externí odkaz:
https://doaj.org/article/2116e83ffc3245f88d1a3ec6d3974ab8
Publikováno v:
Environmental Earth Sciences. 81
The study area of Cala Gonone in NE Sardinia (Italy) consists of a wide terraced re-entrance/valley crowned inland by carbonate hills and, near the coast bounded laterally and partly floored by thin basaltic lava lying over carbonate bedrock. In this
Publikováno v:
Geomorphology. 75:212-225
During deglaciation, the Laurentide Ice Sheet developed lobate ice termini in the Great Lakes area. Where the lobes remained quasi-stationary for considerable time and sediment was supplied by the glacier, end moraines fronted by outwash plains were
Publikováno v:
Canadian Journal of Remote Sensing. 27:143-158
RESUMELes objectifs de cette etude sont : d'analyser la reponse de la retrodiffusion de RADARSAT aux changements saisonniers dans les zones humides du sud des basses terres de la baie d'Hudson, dans le nord de l'Ontario, et d'evaluer le potentiel des
Publikováno v:
International Journal of Coal Geology. 41:213-238
Peat profiles were sampled from a raised bog and an interior fen located in the boreal James Bay Lowlands, Northern Ontario, and a cold-temperate swamp and a cold-temperate bog in the Great Lakes–St. Lawrence Lowlands, southern Ontario. An examinat
Autor:
Michael E. Brookfield, I. P. Martini
Publikováno v:
Sedimentary Geology. 123:183-197
Sequence architecture is controlled by two fundamental factors; the water level relative to the depositional surface (which controls accommodation space), and the points or areas of sediment injection (which control how this space is filled in). Rela
Publikováno v:
Canadian Journal of Earth Sciences. 35:702-719
The Upper Ordovician Queenston Formation constitutes the westernmost part of the Taconic clastic wedge of eastern North America. In Ontario, the Queenston Formation consists of a mixed terrigenous-carbonate succession composed primarily of red silty
Publikováno v:
Sedimentary Geology. 99:37-59
Well exposed, diamond-line cut, quarry-exposures of the Manciano Sandstone allow a detailed analysis of sandy, fossiliferous, nearshore deposits of the shelf of the Northern Apennines. The Manciano Sandstone is characterized by medium to very coarse,
Autor:
M. Sagri, I. P. Martini
Publikováno v:
Earth-Science Reviews. 34:197-233
Extensional and compressional regimes exist at the same time in adjacent parts of the Northern Apennines (Italy), and the former regime succeeded the latter at the same place as the thrust mountain front moved eastward since Miocene times. Numerous e
Siliciclastic-carbonate sequences of Miocene grabens of northern Sardinia, western Mediterranean sea
Publikováno v:
Sedimentary Geology. 76:63-78
The small crustal block of Sardinia Island (western Mediterranean) underwent major rifting events during Oligocene-Early Miocene (Aquitanian), Early Burdigalian, and Plio-Pleistocene times. Sedimentation in the resulting extensional and transtensiona