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  Subjects -> EARTH SCIENCES (Total: 650 journals)
    - EARTH SCIENCES (469 journals)
    - GEOLOGY (72 journals)
    - GEOPHYSICS (27 journals)
    - HYDROLOGY (21 journals)
    - OCEANOGRAPHY (61 journals)

EARTH SCIENCES (469 journals)                  1 2 3 4 5 | Last

Acta Geodaetica et Geophysica     Hybrid Journal   (Followers: 1)
Acta Geodaetica et Geophysica Hungarica     Full-text available via subscription   (Followers: 3)
Acta Geophysica     Open Access   (Followers: 8)
Acta Geotechnica     Hybrid Journal   (Followers: 8)
Acta Meteorologica Sinica     Hybrid Journal   (Followers: 4)
Advances in High Energy Physics     Open Access   (Followers: 16)
Advances In Physics     Hybrid Journal   (Followers: 10)
Aeolian Research     Hybrid Journal   (Followers: 3)
African Journal of Aquatic Science     Hybrid Journal   (Followers: 12)
Algological Studies     Full-text available via subscription   (Followers: 2)
Alpine Botany     Hybrid Journal   (Followers: 5)
AMBIO     Hybrid Journal   (Followers: 13)
Anadolu University Journal of Science and Technology     Open Access  
Anales del Instituto de la Patagonia     Open Access   (Followers: 1)
Andean geology     Open Access   (Followers: 4)
Annales Henri Poincaré     Hybrid Journal   (Followers: 2)
Annales UMCS, Geographia, Geologia, Mineralogia et Petrographia     Open Access   (Followers: 2)
Annals of Geophysics     Full-text available via subscription   (Followers: 11)
Annals of GIS     Hybrid Journal   (Followers: 19)
Annals of Glaciology     Full-text available via subscription   (Followers: 2)
Annual Review of Marine Science     Full-text available via subscription   (Followers: 13)
Anthropocene     Hybrid Journal   (Followers: 1)
Anthropocene Review     Hybrid Journal   (Followers: 4)
Applied Clay Science     Hybrid Journal   (Followers: 3)
Applied Geochemistry     Hybrid Journal   (Followers: 9)
Applied Geomatics     Hybrid Journal   (Followers: 5)
Applied Geophysics     Hybrid Journal   (Followers: 9)
Applied Ocean Research     Hybrid Journal   (Followers: 6)
Applied Petrochemical Research     Open Access   (Followers: 3)
Applied Remote Sensing Journal     Open Access   (Followers: 13)
Aquatic Conservation Marine and Freshwater Ecosystems     Hybrid Journal   (Followers: 36)
Arctic Science     Open Access   (Followers: 7)
Arctic, Antarctic, and Alpine Research     Full-text available via subscription   (Followers: 10)
Artificial Satellites : The Journal of Space Research Centre of Polish Academy of Sciences     Open Access   (Followers: 14)
Asia-Pacific Journal of Atmospheric Sciences     Hybrid Journal   (Followers: 4)
Asian Journal of Earth Sciences     Open Access   (Followers: 22)
Asian Review of Environmental and Earth Sciences     Open Access   (Followers: 1)
Atlantic Geology : Journal of the Atlantic Geoscience Society / Atlantic Geology : revue de la Société Géoscientifique de l'Atlantique     Full-text available via subscription   (Followers: 3)
Atmosphere-Ocean     Full-text available via subscription   (Followers: 7)
Atmospheric and Climate Sciences     Open Access   (Followers: 16)
Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia     Hybrid Journal   (Followers: 12)
Boletim de Ciências Geodésicas     Open Access  
Boreas: An International Journal of Quaternary Research     Hybrid Journal   (Followers: 11)
Bragantia     Open Access   (Followers: 2)
Bulletin of Earthquake Engineering     Hybrid Journal   (Followers: 10)
Bulletin of Geosciences     Open Access   (Followers: 11)
Bulletin of the Lebedev Physics Institute     Hybrid Journal   (Followers: 1)
Bulletin of the Seismological Society of America     Full-text available via subscription   (Followers: 18)
Bulletin of Volcanology     Hybrid Journal   (Followers: 18)
Cadernos de Geociências     Open Access  
Canadian Journal of Plant Science     Full-text available via subscription   (Followers: 15)
Canadian Mineralogist     Full-text available via subscription   (Followers: 3)
Canadian Water Resources Journal     Hybrid Journal   (Followers: 21)
Carbonates and Evaporites     Hybrid Journal   (Followers: 4)
CATENA     Hybrid Journal   (Followers: 5)
Chemical Geology     Hybrid Journal   (Followers: 12)
Chemie der Erde - Geochemistry     Hybrid Journal   (Followers: 4)
Chinese Geographical Science     Hybrid Journal   (Followers: 5)
Chinese Journal of Geochemistry     Hybrid Journal   (Followers: 3)
Chinese Journal of Oceanology and Limnology     Hybrid Journal   (Followers: 2)
Ciencia del suelo     Open Access   (Followers: 2)
Ciencias Espaciales     Open Access  
Climate and Development     Hybrid Journal   (Followers: 12)
Coastal Management     Hybrid Journal   (Followers: 24)
Cogent Geoscience     Open Access  
Comptes Rendus Geoscience     Full-text available via subscription   (Followers: 7)
Computational Geosciences     Hybrid Journal   (Followers: 14)
Computational Mathematics and Mathematical Physics     Hybrid Journal   (Followers: 1)
Computers and Geotechnics     Hybrid Journal   (Followers: 8)
Contemporary Trends in Geoscience     Open Access   (Followers: 2)
Continental Shelf Research     Hybrid Journal   (Followers: 8)
Contributions to Mineralogy and Petrology     Hybrid Journal   (Followers: 10)
Contributions to Plasma Physics     Hybrid Journal   (Followers: 2)
Coral Reefs     Hybrid Journal   (Followers: 16)
Cretaceous Research     Hybrid Journal   (Followers: 6)
Cybergeo : European Journal of Geography     Open Access   (Followers: 3)
Depositional Record     Open Access  
Developments in Geotectonics     Full-text available via subscription   (Followers: 3)
Developments in Quaternary Science     Full-text available via subscription   (Followers: 3)
Développement durable et territoires     Open Access   (Followers: 2)
Diatom Research     Hybrid Journal  
Doklady Physics     Hybrid Journal   (Followers: 1)
Dynamics of Atmospheres and Oceans     Hybrid Journal   (Followers: 4)
E&S Engineering and Science     Open Access  
E3S Web of Conferences     Open Access  
Earth and Planetary Science Letters     Hybrid Journal   (Followers: 78)
Earth and Space Science     Open Access   (Followers: 2)
Earth Interactions     Full-text available via subscription   (Followers: 11)
Earth Science Research     Open Access   (Followers: 7)
Earth Surface Dynamics (ESurf)     Open Access   (Followers: 3)
Earth Surface Processes and Landforms     Hybrid Journal   (Followers: 19)
Earth System Dynamics     Open Access   (Followers: 7)
Earth System Dynamics Discussions     Open Access   (Followers: 4)
Earth's Future     Open Access   (Followers: 1)
Earth, Planets and Space     Open Access   (Followers: 6)
Earthquake Engineering and Engineering Vibration     Hybrid Journal   (Followers: 7)
Earthquake Science     Hybrid Journal   (Followers: 9)
Earthquake Spectra     Full-text available via subscription   (Followers: 16)
Ecohydrology     Hybrid Journal   (Followers: 9)
Ecological Questions     Open Access   (Followers: 6)

        1 2 3 4 5 | Last

Journal Cover Developments in Geotectonics
  [3 followers]  Follow
    
   Full-text available via subscription Subscription journal
   ISSN (Print) 0419-0254
   Published by Elsevier Homepage  [2805 journals]
  • Further Titles in this Series
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22




      PubDate: 2013-11-06T13:30:07Z
       
  • Front Matter
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22




      PubDate: 2013-11-06T13:30:07Z
       
  • Copyright page
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22




      PubDate: 2013-11-06T13:30:07Z
       
  • Preface
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22
      Author(s): WARREN MANSPEIZER



      PubDate: 2013-11-06T13:30:07Z
       
  • List of Contributors
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22




      PubDate: 2013-11-06T13:30:07Z
       
  • Chapter 1 Variscan – Alleghanian orogen
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22
      Author(s): N. RAST
      The Variscan – Alleghanian orogen stretches from the southeastern United States to eastern Europe and fragments of it are also detected in eastern and northeastern Africa. The orogen has originally been produced by the collision between Gondwana, Laurentian and Baltic cratons, as well as the intervening microcontinents. As a result of postorogenic erosion, superposed sedimentation and Mesozic and Tertiary rifting and compressive episodes the orogen is divided into separated segments and massifs. The north-northwestern edge of the orogen, marked by the northern Variscan thrust and deformation front, indicates tectonic transport to the north-northwest, while the south-southeastern edge of the orogen similarly delineated by the southern Variscan front shows tectonic transport to the south-southeast. This polarity is the strongest evidence for the continental collision causing Variscan – Alleghanian orogeny. Within the fronts the orogen can be divided into the internides and the northern and southern externides. The internides are characterized by variable, but commonly high-grade metamorphism and granitic intrusions. The northern externides are weakly metamorphosed, generally devoid of granites, and strongly affected by overthrusting. The southern externides have had similar features but are heavily overprinted by the Alpine structures. Several lines can be suggested as collisional sutures. The orogen forms a foundation to the postorogenic Permo-Triassic deposits.


      PubDate: 2013-11-06T13:30:07Z
       
  • Chapter 2 Triassic – Jurassic plate migrations and paleogeographic
           reconstructions in the Atlantic domain
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22
      Author(s): ROB VAN DER VOO
      New insights into the Triassic paleomagnetic data base for the Atlantic-bordering continents, coupled with a previously published analysis of late Paleozoic paleopoles, reveal that of all the different Pangea reconstructions, a fit in which northwestern South America and the Gulf Coast of North America are juxtaposed best matches the available data. This fit has previously been referred to as Pangea A2. Other models (Pangea B, C) are not supported by the paleomagnetic and geological data. Latest Triassic – Early Jurassic paleopoles for North America's Colorado Plateau from the Wingate and Chinle Formations fall near 60°N, 62°E; when African paleopoles of the same age are compared with this pair, the best rotation parameters to bring them into agreement are also in support of Pangea A2. This implies that the early opening of the central North Atlantic Ocean and the Gulf of Mexico occurred from an initial reconstruction such as Pangea A2.


      PubDate: 2013-11-06T13:30:07Z
       
  • Chapter 3 Triassic – Jurassic rifting and opening of the Atlantic:
           An overview
    • Abstract: Publication date: 1988
      Source:Developments in Geotectonics, Volume 22
      Author(s): WARREN MANSPEIZER
      Events leading to the breakup of the Pangean plate and evolution of the Atlantic passive margins are recorded in the rock record of more than 40 offshore and onshore Late Triassic – Early Jurassic synrift basins that formed on the Variscan – Alleghanian orogen. The record shows that rifting took place along low-angle detachment faults, giving rise to half-grabens along a conjugate set of lower and upper plate margins that are noteably asymmetric. The American plate was marked by a broad belt of marginal plateaus with many northeast-trending detrital basins that were linked to eachother by transfer faults and displaced by cross faults. The Moroccan plate, on the other hand, was marked by few broadly subsiding evaporite basins. Typically each half-graben on the American plate was bordered by a hinged margin and one major basin-bounding fault, which delineated the surface trace of synthetic or antithetic listric faults on a seaward-dipping detachment zone. The American plate (during the Late Triassic) was dominated by high relief with high-altitude fluvial-lacustrine basins along the western part of the orogen, and by low-relief sea-level evaporite basins proximal to the future spreading axis. During detachment faulting, in the Late Triassic – Early Jurassic, the lower plate must have been uplifted isostatically into a broad central arch that migrated seaward, as the load of the overlying upper plate continued to be reduced by erosion and listric faulting. This had the consequence of elevating Late Triassic marine strata that lay near the proto-Atlantic axis. During the Lias, these marine basins were eroded and their strata reworked and transported landward toward the onshore basins of Morocco and North America. The topographic reversal is thought to reflect the easterly migration of upwelling asthenosphere, in response to tectonic thinning along the newly forming margin. It was a time of major crustal thinning with development of the postrift unconformity (COST G-2 cores), and adiabatic decompression on the upwelling asthenosphere. Whereas the earliest melts yielded off-axis alkaline-rich volcanics (as in Morocco), subsequent melts, which were derived from later partial melt derivatives, were tholeiitic (as in the Palisades). As the upwelling asthenosphere migrated eastward in response to tectonic thinning, the ‘abandoned’ rift-stage crust cooled and subsided, thereby ushering in the drifting phase of the margin. The Moroccan plate, by contrast, was a broad region of low relief throughout most of the Triassic and Liassic. It was distinguished by few detrital basins, and almost all of these occurred along the South Atlas fracture zone, as Triassic strike-slip basins in the High Atlas. Except for the offshore Essaouira basin, which is a seaward extension of the High Atlas Argana basin, the Moroccan margin (unlike the American) consists of few documented Triassic – Liassic rift basins. Triassic rifting of the Middle Atlas (e.g. at Bab-Bou-Idir and Berkane) broke the orogen into the Oranian and Moroccan mesetas, and is manifested by a thick carbonate sequence. The majority of the intraplate basins of North African occur on the mesetas, and are nonrift; typically they contain nonclastic, marine and fresh water evaporites of Liassic and younger strata that formed in broad, shallow, drift-type basins on a generally subsiding terrane of low relief, near the very end of synrift time.


      PubDate: 2013-11-06T13:30:07Z
       
 
 
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