1 edition of The Paleogene and Neogene of Western Iberia (Portugal) found in the catalog.
The Paleogene and Neogene of Western Iberia (Portugal)
|Statement||by João Pais|
|Series||SpringerBriefs in Earth Sciences|
|Contributions||SpringerLink (Online service)|
|The Physical Object|
|Format||[electronic resource] :|
|ISBN 10||9783642224003, 9783642224010|
The Neogene (/ ˈ n iː. ə ˌ dʒ iː n, ˈ n iː. oʊ-/ NEE-ə-jeen, NEE-oh-) (informally Upper Tertiary or Late Tertiary) is a geologic period and system that spans million years from the end of the Paleogene Period million years ago to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later g: Western Iberia. Reliable palaeomagnetic data from the emerged margins of the Valencia trough include results from Triassic, Jurassic, Paleogene and Miocene rocks. From these data, a clockwise rotation of the Catalan Coastal ranges relative to the western part of Iberia is apparent. In addition, a clockwise rotation is indicated by the magnetic directions from the Balearics with respect to those of the Catalan.
Most of western California was still underwater during the Paleogene, as evidenced by marine fossils, but continued to form and emerge throughout the Cenozoic. Fossil evidence indicates the first archaic mammals appeared in the Jurassic Period of the Mesozoic, approximately – Ma. Mammalia and Aves, evolutionarily constrained by predation and competition from non-avian Archosaurians. The Paleogene (/ ˈ p æ l. i. ə ˌ dʒ iː n,-i. oʊ-, ˈ p eɪ. l i-,-l i. oʊ-/ PAL-ee-ə-jeen, -ee-oh-, PAY-lee-, -lee-oh-; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period 66 million years ago to the beginning of the Neogene Period g: Western Iberia.
The first paper details our findings east of Turkey beneath the southern Caspian Sea. 1 Here, we found about 17 km ( mi) of Tertiary (Paleogene and Neogene) strata covering an area over miles wide. This is one of the thickest deposits of Tertiary sediment in the world, and all of it was deposited on top of Cretaceous and older rocks. Paleogene gas reservoirs in the Yingmai7 gas field contain high content of total hydrocarbon and low content of nonhydrocarbon (generally less than 5%). The aridity coefficient mainly varies from – (Table ).CH 4 content is –% and C 2 H 6 content is –%, indicating wet gas. In nonhydrocarbon gas, N 2 content is –%, and CO 2 content is –%.Missing: Western Iberia.
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The Paleogene and Neogene of Western Iberia (Portugal) A Cenozoic record in the European Atlantic domain. Authors: Pais, João Free PreviewBrand: Springer-Verlag Berlin Heidelberg.
The Paleogene and Neogene of Western Iberia (Portugal): A Cenozoic record in the European Atlantic domain (SpringerBriefs in Earth Sciences) th Edition by João Pais Price: $ The Paleogene and Neogene of Western Iberia (Portugal): A Cenozoic Record in the European Atlantic Domain João Pais, Pedro P.
Cunha, Diamantino Pereira, Paulo Legoinha, Rúben Dias, Delminda Moura et al. Pages The Paleogene and Neogene of Western Iberia (Portugal). [João Pais] -- This volume includes a general description of the Portuguese Cenozoic basins in the Iberian tectonic context.
The main stratigraphic units, including sedimentological, stratigraphical and. The Paleogene and Neogene of western Iberia (Portugal): a Cenozoic record in the European Atlantic domain.
[João José Cardoso Pais;] Book, Internet Resource: All Authors / Contributors: João José Cardoso Pais. Find more information about: ISBN:.
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The Paleogene and Neogene of Western Iberia (Portugal) pp | Cite as The Paleogene and Neogene of Western Iberia (Portugal): A Cited by: The Paleogene and Neogene of Western Iberia (Portugal) eBook por João Pais - | Rakuten Kobo Lee "The Paleogene and Neogene of Western Iberia (Portugal) A Cenozoic record in the European Atlantic domain" por João Pais disponible en Rakuten Kobo.
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CHAPTER 5 - NEOGENE TECTONIC EVOLUTION OF THE IBERIAN PENINSULA AND WESTERN MEDITERRANEAN In this chapter the geological evolution of the study area from the Neogene up to present is presented in the same way as the Paleogene evolution has been described in the previous chapter, in maps for every 3Ma.
The major tectonic events during the Neogene. Over the last 65 Ma, our world assumed its modern shape. This timespan is divided into the Palaeogene Period, lasting from 65 to 23 Ma and the Neogene, which extends up to the present day (see Gradstein & Ogg () and Gregory et al.
() for discussion about the Quaternary). Throughout the Cenozoic Era, Africa was moving towards Eurasia in a northward direction and with a counterclockwise Missing: Western Iberia. Later in the Neogene some of them migrated to North America once the Americas were connected at Panama.
Large mammal predators had not yet evolved early in the Paleogene so there was little competition and the big birds dominated. The Oceans And Lakes of the Paleogene. In the oceans, fish species branched out. Sharks became more g: Western Iberia.
The term Paleogene was devised in Europe to emphasize the similarity of marine fossils found in rocks of the first three Cenozoic epochs, as opposed to the later fossils of the Neogene Period (23 million to million years ago) and the Quaternary Period ( million years ago to the present).Missing: Western Iberia.
Figure for northern Africa, the western Mediterranean and the Betic/Alboran region. Figure serves as legend for all the plates of the reconstruction. 65 Ma, KT-boundary, Figure General Along northern Iberia and southern France, inversion of former Mesozoic normal faults occurs and subduction or underthrusting is active.
The Neogene Period Major Changes For The Present Planet Earth. The Neogene Period - Learn The Facts, Climate, Plants, Animals, and The Major Events That Bring The Earth to Its Present Form. This Period, our period began about 24 million years ago and it continues up to the present time.
The name “Neogene” is a new name for part of the old Tertiary Period and includes the old Quaternary Missing: Western Iberia.
Publication date: Janu This Special Report comprehensively describes the stratigraphy and correlation of the Tertiary (Paleogene-Neogene) rocks of NW Europe and the adjacent Atlantic Ocean and is the summation of fifty years of research on Tertiary sediments by Chris g: Western Iberia. This book provides a representative assessment of the state of the art of research on Paleogene rotaliid larger foraminifera.
It gives an overview of the current understanding of systematics of this group and, in particular, of its biostratigraphic importance and palaeobiogeography.
Paleogene Rocks, Hualapai Plateau ‐ Western Grand Canyon. Neogene Rocks, Hualapai Plateau ‐ Western Grand Canyon. Geomorphic Significance of the Eocene(?) ‐ Early Miocene(?) Rocks.
Miocene Volcanism and Related Events: Hualapai Plateau. Post‐Volcanic Sedimentation History. Regional Structural Perspective. Summary and ConclusionsMissing: Western Iberia. Over wide areas the rocks of the Khorat Plateau are flat-lying, but toward the plateau's western and southern rims the rocks dip inwards and are responsible for its broad dish-like structure.
Also, crossing the northern part of the Khorat Plateau is a WNW–ESE trending belt of gentle anticlinal folding, the Phu Phan Uplift (Fig. 1).Missing: Western Iberia. About Gastornis. First things first: the flightless prehistoric bird we now know as Gastornis used to be called Diatryma (Greek for "through a hole"), the name by which it was recognized by generations of schoolchildren.
After examining some fossil specimens unearthed in New Mexico, the famous American paleontologist Edward Drinker Cope coined the name Diatryma innot Missing: Western Iberia. The 43 million years of the Paleogene period represent a crucial interval in the evolution of mammals, birds, and reptiles, which were free to occupy new ecological niches after the demise of the dinosaurs following the K/T Extinction Paleogene was the first period of the Cenozoic Era (65 million years ago to the present), followed by the Neogene period ( million years ago Missing: Western Iberia.The Paleogene/Neogene boundary in continental deposits of the West Siberian Plain.
This paper presents palynological and paleomagnetic characteristics of three West Siberian horizons: Zhuravka (Upper Oligocene, Chattian), Abrosimovka, and Beshcheul (Lower-Middle Miocene, Aquitanian, Burdigalian, Langhian, and Serravallian).Missing: Western Iberia.