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    Cratonic Basin Formation : A Case Study of the Parnaíba Basin of Brazil (2018)
    London : The Geological Society
    Details
    Keywords: basin research ; cratonic basin ; Parnaíba Basin ; Brazil
    Description / Table of Contents: Cratonic basin formation: a case study of the Parnaíba Basin of Brazil / M. C. Daly, R. A. Fuck, J. Julià, D. I. M. Macdonald and A. B. Watts / Geological Society, London, Special Publications, 472, 1-15, 14 September 2018, https://doi.org/10.1144/SP472.20 --- Cratonic basins --- Cratonic basins with reference to the Michigan basin / Norman H. Sleep / Geological Society, London, Special Publications, 472, 17-35, 6 February 2018, https://doi.org/10.1144/SP472.1 --- Lithospheric heating by crustal thickening: a possible origin of the Parnaíba Basin / D. McKenzie and V. Rodríguez Tribaldos / Geological Society, London, Special Publications, 472, 37-44, 19 February 2018, https://doi.org/10.1144/SP472.5 --- A comparative study of the Parnaíba, Michigan and Congo cratonic basins / A. B. Watts, B. Tozer, M. C. Daly and J. Smith / Geological Society, London, Special Publications, 472, 45-66, 22 February 2018, https://doi.org/10.1144/SP472.6 --- The Parnaíba cratonic basin: lithospheric and crustal structure --- Structure of the crust and upper mantle beneath the Parnaíba Basin, Brazil, from wide-angle reflection–refraction data / José E. P. Soares, Randell Stephenson, Reinhardt A. Fuck, Marcus V. A. G. de Lima, Vitto C. M. de Araújo, Flávio T. Lima, Fábio A. S. Rocha and Cíntia R. da Trindade / Geological Society, London, Special Publications, 472, 67-82, 13 April 2018, https://doi.org/10.1144/SP472.9 --- Deep crustal architecture of the Parnaíba basin of NE Brazil from receiver function analysis: implications for basin subsidence / Diogo L. O. Coelho, Jordi Julià, Verónica Rodríguez-Tribaldos and Nicholas White / Geological Society, London, Special Publications, 472, 83-100, 16 May 2018, https://doi.org/10.1144/SP472.8 --- Reprocessing and interpretation of deep structures in a regional transect of the Parnaíba Basin, Brazil / Rafael R. Manenti, Wilker E. Souza and Milton J. Porsani / Geological Society, London, Special Publications, 472, 101-107, 12 June 2018, https://doi.org/10.1144/SP472.17 --- Electrical conductivity structure across the Parnaíba Basin, NE Brazil / F. F. Solon, S. L. Fontes and E. F. La Terra / Geological Society, London, Special Publications, 472, 109-126, 13 July 2018, https://doi.org/10.1144/SP472.19 --- The pre-Silurian Riachão basin: a new perspective on the basement of the Parnaíba basin, NE Brazil / Amanda Porto, Michael C. Daly, Emanuele La Terra and Sergio Fontes / Geological Society, London, Special Publications, 472, 127-145, 19 February 2018, https://doi.org/10.1144/SP472.2 --- Implications of preliminary subsidence analyses for the Parnaíba cratonic basin / Verónica Rodríguez Tribaldos and Nicky White / Geological Society, London, Special Publications, 472, 147-156, 6 February 2018, https://doi.org/10.1144/SP472.3 --- The Parnaíba cratonic basin: stratigraphic and sedimentological evolution --- Evolution of a cratonic basin: insights from the stratal architecture and provenance history of the Parnaíba Basin / L. A. Menzies, A. Carter and David I. M. MacDonald / Geological Society, London, Special Publications, 472, 157-179, 6 August 2018, https://doi.org/10.1144/SP472.18 --- Provenance of sandstones in the Parnaíba Basin through detrital zircon geochronology / M. H. B. M. Hollanda, A. M. Góes and F. A. Negri / Geological Society, London, Special Publications, 472, 181-197, 12 July 2018, https://doi.org/10.1144/SP472.16 --- Palaeogeographical and palaeoclimatic evolution of the intracratonic Parnaíba Basin, NE Brazil using GPlates plate tectonic reconstructions and chemostratigraphic tools / Marwan M. Jaju, Haydon P. Mort, Fadi H. Nader, Mário L. Filho and David I. M. Macdonald / Geological Society, London, Special Publications, 472, 199-222, 6 June 2018, https://doi.org/10.1144/SP472.12 --- Re-evaluation of the Permian macrofossils from the Parnaíba Basin: biostratigraphic, palaeoenvironmental and palaeogeographical implications / Roberto Iannuzzi, Rodrigo Neregato, Juan C. Cisneros, Kenneth D. Angielczyk, Ronny Rößler, Rosemarie Rohn, Claudia Marsicano, Jörg Fröbisch, Thomas Fairchild, Roger M. H. Smith, Francine Kurzawe, Martha Richter, Max C. Langer, Tatiane M. V. Tavares, Christian F. Kammerer, Domingas M. Conceição, Jason D. Pardo and Guilherme A. Roesler / Geological Society, London, Special Publications, 472, 223-249, 2 July 2018, https://doi.org/10.1144/SP472.14 --- The Parnaíba cratonic basin: magmatic history --- Geochemical and temporal provinciality of the magmatism of the eastern Parnaíba Basin, NE Brazil / Monica Heilbron, Eliane Guedes, Miguel Mane, Claudio de Morisson Valeriano, Miguel Tupinambá, Júlio Almeida, Luiz Guilherme do Eirado Silva, Beatriz Paschoal Duarte, Jorge Carlos Dela Favera and Adriano Viana / Geological Society, London, Special Publications, 472, 251-278, 5 June 2018, https://doi.org/10.1144/SP472.11 --- Petrology of Jurassic and Cretaceous basaltic formations from the Parnaíba Basin, NE Brazil: correlations and associations with large igneous provinces / Alisson L. Oliveira, Márcio M. Pimentel, Reinhardt A. Fuck and Diógenes C. Oliveira / Geological Society, London, Special Publications, 472, 279-308, 6 August 2018, https://doi.org/10.1144/SP472.21 --- Role of basaltic magmatism within the Parnaíba cratonic basin, NE Brazil / Marthe Klöcking, Nicky White and John MacLennan / Geological Society, London, Special Publications, 472, 309-319, 23 March 2018, https://doi.org/10.1144/SP472.4 --- Phanerozoic magmatism in the Parnaíba Basin: characterization of igneous bodies (well logs and 2D seismic sections), geometry, distribution and sill emplacement patterns / I. Trosdtorf, J. M. Morais Neto, S. F. Santos, C. V. Portela Filho, T. A. Dall Oglio, A. C. M. Galves and A. M. Silva / Geological Society, London, Special Publications, 472, 321-340, 16 May 2018, https://doi.org/10.1144/SP472.10 --- The Parnaíba cratonic basin: resource system --- Atypical igneous-sedimentary petroleum systems of the Parnaíba Basin, Brazil: seismic, well logs and cores / Frederico S. de Miranda, Ana Luiza Vettorazzi, Paulo R. da Cruz Cunha, Fernando B. Aragão, Diogo Michelon, João Luiz Caldeira, Ernani Porsche, Celso Martins, Roberto B. Ribeiro, Alexandre F. Vilela, José R. Corrêa, Lilian S. Silveira and Kátia Andreola / Geological Society, London, Special Publications, 472, 341-360, 12 July 2018, https://doi.org/10.1144/SP472.15 --- New insights into the Parnaíba Basin: results of investments by the Brazilian National Petroleum Agency / Marina Abelha, Eliane Petersohn, Gabriel Bastos and Daniel Araújo / Geological Society, London, Special Publications, 472, 361-366, 5 July 2018, https://doi.org/10.1144/SP472.13
    Pages: Online-Ressource (VIII, 372 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203960
    URL: https://sp.lyellcollection.org/content/472/1
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Nutritional Variation in Cottonseed, Effect of Autoclaving in Presence and Absence of Gossypol on Solvent Extracted Cottonseed Meal (1954)
    s.l. : American Chemical Society
    Journal of agricultural and food chemistry 2 (1954), S. 822-826 
    Details
    ISSN: 1520-5118
    Source: ACS Legacy Archives
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/jf60036a003
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  • 3
    Electronic Resource
    Electronic Resource
    The Great Glen Fault in the Shetland Area (1970)
    [s.l.] : Nature Publishing Group
    Nature 227 (1970), S. 268-269 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Flinn has suggested a new line for the Great Glen fault which does not cross gravity "high" A north of the Shet-lands. This raises a problem which needs to be recognized. To quote Allen5, "probably the most impressive feature of thoroughgoing transcurrent faults is their extreme linearity over ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/227268b0
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  • 4
    Electronic Resource
    Electronic Resource
    Crustal structure, gravity anomalies and flexure of the lithosphere in the vicinity of the Canary Islands (1994)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 119 (1994), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Simple elastic plate models have been used to calculate the flexure of the lithosphere caused by volcanic loading at the Canary Islands and sediment loading at the Moroccan continental margin. By comparing the calculated flexure to observations based on seismic refraction and free-air gravity anomaly data, constraints have been placed on the long-term (〉106 years) elastic thickness of the lithosphere, Te. The best fit between the calculated and observed flexure in the vicinity of the Canary Islands is for Te= 20 km. This value of Te also explains seismic reflection data in regions that flank the island provided that the lithosphere underlying the Moroccan margin is sufficiently weak (Te 〈 5 km) for sediment loading to contribute little to the island flexure. a backstripping study, in which gravity data are used to constrain the value of Te, supports the suggestion that the lithosphere underlying the Moroccan margin, like its conjugate at the Baltimore Canyon Trough, is weak. Although sediment loading at the Moroccan margin appears therefore to have exerted little influence on the structure of the Canary Islands, there is evidence that island flexure may have influenced the stratigraphic development of the Moroccan margin, especially in the region of the ‘slope anticline’. A Te, of 20 km is about 15 km lower than would be expected on the basis of the thermal age of the oceanic lithosphere that underlies the Canary Islands. Similar low values have been reported from oceanic islands in the Pacific ‘superswell’ region of French Polynesia where they have been attributed to re-heating of the lithosphere by one or more hotspots. A general E-W age progression of the volcanic rocks suggests that the Canary Islands were also generated by a hotspot. They lack, however, the topographic swell and gravity/geoid high which usually accompanies these features. One possibility is that the low Te values are the result of a pre-existing weakness in the oceanic crust. A Te of 20 km is large enough, however, for a significant part of the mantle to still be involved in the support of the island loads. A more likely explanation is thermal weakening by a hotspot which has been localized enough to reduce Te but not to produce a swell or gravity/geoid high. Irrespective of its cause, the low Te suggests that oceanic lithosphere does not necessarily progressively increase its strength with age, so that even 140 Ma old lithosphere is vulnerable and can, in some regions, be significantly weakened by later thermal and mechanical processes.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1994.tb00147.x
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  • 5
    Electronic Resource
    Electronic Resource
    Moho and lower crustal reflectivity beneath a young rift basin: results from a two-ship, wide-aperture seismic-reflection experiment in the Valencia Trough (western Mediterranean) (1994)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 118 (1994), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We present new images of the lower crust and Moho beneath the Valencia Trough—a young rift basin in the western Mediterranean. These images were obtained from a two-ship, wide-aperture reflection experiment and show several features not distinguishable on previously available conventional single-ship reflection profiles.The Moho, which was previously only seen intermittently, can now be confidently traced throughout the basin. We have constructed a present-day depth-to-Moho map and estimated the degree of crustal thinning for the whole basin. Crustal thinning is at a maximum in the centre of the basin, where β values reach 3.15 ± 0.25. At the margins of the basin the β value decreases to 1.5 ± 0.1.The reflective character of the lower crust and Moho is different beneath different parts of the basin. We have been able to correlate these differences with the amount of stretching. We therefore interpret the variations of the observed lower crustal reflectivity as having been caused by the most recent (Neogene) stretching event that opened the Valencia Trough. Along the Iberian margin there is well-developed lower crustal reflectivity consisting of 1-2s two-way time (TWT) of 1-4 km long, near-horizontal reflectors underlain by a more continuous, although not significantly stronger, reflector interpreted to be the reflection Moho. Offshore, this lower crustal reflective unit thins rapidly, such that it is undetectable 40-50 km from the coastline where the crust has been stretched by a factor of 1.7 ± 0.1. As the lower crustal reflectivity becomes undetectable the reflection Moho becomes a robust, continuous event. Where β exceeds 2.4 ± 0.2, however, the Moho is a weak event and difficult to trace. We infer that either the extension itself or associated melting significantly weakened or even destroyed the lower crustal reflectivity in the centre of the basin and enhanced the Moho where extension was moderate.The Balearic margin is somewhat anomalous in that there appears to have been flexural loading of the crust due to thrusting and folding that occurred at the same time as extension in the Valencia Trough. The lower crust shows evidence of weak, but locally variable lower crustal reflectivity. It is possible that the lower crustal reflectivity was preserved simply because the Moho was flexed downward and so decompression, and hence melting, of the upper mantle was restricted. This suggests that the melting itself rather than the extension is the primary mechanism of lower crustal modification.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1994.tb04681.x
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  • 6
    Electronic Resource
    Electronic Resource
    Long Wavelength Gravity and Topography Anomalies (1981)
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 9 (1981), S. 415-448 
    Details
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1146/annurev.ea.09.050181.002215
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  • 7
    Electronic Resource
    Electronic Resource
    The long-term strength of Europe and its implications for plate-forming processes (2005)
    [s.l.] : Macmillian Magazines Ltd.
    Nature 436 (2005), S. 381-384 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Field-based geological studies show that continental deformation preferentially occurs in young tectonic provinces rather than in old cratons. This partitioning of deformation suggests that the cratons are stronger than surrounding younger Phanerozoic provinces. However, although Archaean and ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/nature03854
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  • 8
    Electronic Resource
    Electronic Resource
    Tectonic subsidence, flexure and global changes of sea level (1982)
    [s.l.] : Nature Publishing Group
    Nature 297 (1982), S. 469-474 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Tectonic models for the evolution of passive continental margins predict that following rifting, sediments should progressively onlap basement at the edge of a margin as the lithosphere cools and increases its flexural rigidity with age. The pattern of modelled onlap is strikingly similar to that ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/297469a0
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  • 9
    Electronic Resource
    Electronic Resource
    Deep Sedimentary Basins proved in the Shetland–Hebridean Continental Shelf and Margin (1970)
    [s.l.] : Nature Publishing Group
    Nature 225 (1970), S. 265-268 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The regional rise in Bouguer anomaly across the shelf towards the continental margin is shown in Fig. 2. This is attributed to the thinning of the crust beneath the slope, from a continental type beneath the shelf to a thinner crust beneath the Shetland?Faroe channel, in quantitative agreement with ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/225265a0
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  • 10
    Electronic Resource
    Electronic Resource
    Seismic stratigraphy of the flexural moat flanking the Hawaiian Islands (1985)
    [s.l.] : Nature Publishing Group
    Nature 317 (1985), S. 421-424 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Figure 1 shows common mid-point (CMP) multichannel seismic reflection line 314 of the flexural moat NNE of Oahu, Hawaii. Individual traces were demuxed, gathered and stacked in 50-m bins7. Predictive deconvolution was applied after stacking and the data were bandpass filtered (6-30 Hz). Although ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/317421a0
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