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  • 1
    Keywords: Salztektonik ; Salze ; Diapirs ; Evaporite ; Salt tectonics ; Sel
    Description / Table of Contents: Ian Davison, Ian Alsop, and Derek Blundell: Salt tectonics: some aspects of deformation mechanics / Geological Society, London, Special Publications, 100:1-10, doi:10.1144/GSL.SP.1996.100.01.01 --- Outcrop, Mine and Borehole Studies --- Stanisław Burliga: Kinematics within the Kłodawa salt diapir, central Poland / Geological Society, London, Special Publications, 100:11-21, doi:10.1144/GSL.SP.1996.100.01.02 --- Ian Davison, Dan Bosence, G. Ian Alsop, and Mohammed H. Al-Aawah: Deformation and sedimentation around active Miocene salt diapirs on the Tihama Plain, northwest Yemen / Geological Society, London, Special Publications, 100:23-39, doi:10.1144/GSL.SP.1996.100.01.03 --- Amos Frumkin: Uplift rate relative to base-levels of a salt diapir (Dead Sea Basin, Israel) as indicated by cave levels / Geological Society, London, Special Publications, 100:41-47, doi:10.1144/GSL.SP.1996.100.01.04 --- Manuel Hoyos, Miguel Doblas, Sergio Sánchez-Moral, Juan Carlos Cañaveras, Salvador Ordoñez, Carmen Sesé, Enrique Sanz, and Vicente Mahecha: Hydration diapirism: a climate-related initiation of evaporite mounds in two continental Neogene basins of central Spain / Geological Society, London, Special Publications, 100:49-63, doi:10.1144/GSL.SP.1996.100.01.05 --- M. Sans, A. L. Sánchez, and P. Santanach: Internal structure of a detachment horizon in the most external part of the Pyrenean fold and thrust belt (northern Spain) / Geological Society, London, Special Publications, 100:65-76, doi:10.1144/GSL.SP.1996.100.01.06 --- Denys B. Smith: Deformation in the late Permian Boulby Halite (EZ3Na) in Teesside, NE England / Geological Society, London, Special Publications, 100:77-87, doi:10.1144/GSL.SP.1996.100.01.07 --- C. J. Talbot and M. Alavi: The past of a future syntaxis across the Zagros / Geological Society, London, Special Publications, 100:89-109, doi:10.1144/GSL.SP.1996.100.01.08 --- Regional Case Studies --- Peter G. Buchanan, Daniel J. Bishop, and David N. Hood: Development of salt-related structures in the Central North Sea: results from section balancing / Geological Society, London, Special Publications, 100:111-128, doi:10.1144/GSL.SP.1996.100.01.09 --- H. S. Edgell: Salt tectonism in the Persian Gulf Basin / Geological Society, London, Special Publications, 100:129-151, doi:10.1144/GSL.SP.1996.100.01.10 --- Fivos Spathopoulos: An insight on salt tectonics in the Angola Basin, South Atlantic / Geological Society, London, Special Publications, 100:153-174, doi:10.1144/GSL.SP.1996.100.01.11 --- S. A. Stewart, M. J. Harvey, S. C. Otto, and P. J. Weston: Influence of salt on fault geometry: examples from the UK salt basins / Geological Society, London, Special Publications, 100:175-202, doi:10.1144/GSL.SP.1996.100.01.12 --- Max Zirngast: The development of the Gorleben salt dome (northwest Germany) based on quantitative analysis of peripheral sinks / Geological Society, London, Special Publications, 100:203-226, doi:10.1144/GSL.SP.1996.100.01.13 --- Physical Modelling --- G. Ian Alsop: Physical modelling of fold and fracture geometries associated with salt diapirism / Geological Society, London, Special Publications, 100:227-241, doi:10.1144/GSL.SP.1996.100.01.14 --- H. Koyi: Salt flow by aggrading and prograding overburdens / Geological Society, London, Special Publications, 100:243-258, doi:10.1144/GSL.SP.1996.100.01.15 --- P. Szatmari, M. C. M. Guerra, and M. A. Pequeno: Genesis of large counter-regional normal fault by flow of Cretaceous salt in the South Atlantic Santos Basin, Brazil / Geological Society, London, Special Publications, 100:259-264, doi:10.1144/GSL.SP.1996.100.01.16 --- Numerical and Geophysical Modelling --- Harvey A. Cohen and Stuart Hardy: Numerical modelling of stratal architectures resulting from differential loading of a mobile substrate / Geological Society, London, Special Publications, 100:265-273, doi:10.1144/GSL.SP.1996.100.01.17 --- K. Petersen and I. Lerche: Temperature dependence of thermal anomalies near evolving salt structures: importance for reducing exploration risk / Geological Society, London, Special Publications, 100:275-290, doi:10.1144/GSL.SP.1996.100.01.18 --- Alexei N. B. Poliakov, Yuri Yu. Podladchikov, Ethan Ch. Dawson, and Christopher J. Talbot: Salt diapirism with simultaneous brittle faulting and viscous flow / Geological Society, London, Special Publications, 100:291-302, doi:10.1144/GSL.SP.1996.100.01.19
    Pages: Online-Ressource (310 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1897799446
    Language: English
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  • 2
    Keywords: sedimentary basins; orogenic belts; petroleum geology; Mexico; Florida; Caribbean
    Description / Table of Contents: The basins, orogens and evolution of the southern Gulf of Mexico and Northern Caribbean / Ian Davison, James Pindell and Jonathan Hull / Geological Society, London, Special Publications, 504, 1-27, 18 December 2020, https://doi.org/10.1144/SP504-2020-218 --- A revised synthesis of the rift and drift history of the Gulf of Mexico and surrounding regions in the light of improved age dating of the Middle Jurassic salt / James Pindell, Diego Villagómez, Roberto Molina-Garza, Rod Graham and Bodo Weber / Geological Society, London, Special Publications, 504, 29-76, 1 October 2020, https://doi.org/10.1144/SP504-2020-43 --- Crustal origin of the West Florida Terrane, and detrital zircon provenance and development of accommodation during initial rifting of the southeastern Gulf of Mexico and western Bahamas / R. N. Erlich and J. Pindell / Geological Society, London, Special Publications, 504, 77-118, 27 August 2020, https://doi.org/10.1144/SP504-2020-14 --- The Sureste Basin of Mexico: its framework, future oil exploration opportunities and key challenges ahead / Mark V. Shann / Geological Society, London, Special Publications, 504, 119-146, 30 July 2020, https://doi.org/10.1144/SP504-2019-214 --- Salt tectonics in the Sureste Basin, SE Mexico: some implications for hydrocarbon exploration / Ian Davison / Geological Society, London, Special Publications, 504, 147-165, 27 August 2020, https://doi.org/10.1144/SP504-2019-227 --- Provenance of the Miocene Nanchital conglomerate, western Chiapas Foldbelt, Mexico: implications for reservoir sands in the Sureste Basin, Greater Campeche Province / James Pindell, Roberto Molina-Garza, Diego Villagómez, Uwe Martens, Rod Graham, Daniel Stockli, Bodo Weber and María Isabel Sierra-Rojas / Geological Society, London, Special Publications, 504, 167-182, 6 July 2020, https://doi.org/10.1144/SP504-2020-12 --- Regional geological analysis of the southern deep Gulf of Mexico and northern Yucatán Shelf / Ernesto Miranda-Madrigal and Gabriel Chávez-Cabello / Geological Society, London, Special Publications, 504, 183-202, 22 September 2020, https://doi.org/10.1144/SP504-2020-1 --- Regional thermal maturity modelling of hydrocarbons along the deep-water Yucatan margin, southern Gulf of Mexico / J. J. Kenning and Paul Mann / Geological Society, London, Special Publications, 504, 203-231, 27 July 2020, https://doi.org/10.1144/SP504-2019-252 --- Palaeogeographical reconstruction and provenance of Oxfordian aeolian sandstone reservoirs in Mexico offshore areas: comparison to the Norphlet aeolian system of the northern Gulf of Mexico / John W. Snedden, D. F. Stockli and I. O. Norton / Geological Society, London, Special Publications, 504, 233-253, 9 July 2020, https://doi.org/10.1144/SP504-2019-219 --- Late Mesozoic and Cenozoic thermotectonic history of eastern, central and southern Mexico as determined through integrated thermochronology, with implications for sediment delivery to the Gulf of Mexico / Gary G. Gray, Diego Villagomez, James Pindell, Roberto Molina-Garza, Paul O'Sullivan, Daniel Stockli, William Farrell, David Blank and Jonathan Schuba / Geological Society, London, Special Publications, 504, 255-283, 23 July 2020, https://doi.org/10.1144/SP504-2019-243 --- Integrated Cretaceous–Cenozoic plate tectonics and structural geology in southern Mexico / Rod Graham, James Pindell, Diego Villagómez, Roberto Molina-Garza, James Granath and Maria Sierra-Rojas / Geological Society, London, Special Publications, 504, 285-314, 24 November 2020, https://doi.org/10.1144/SP504-2020-70 --- Illite 40Ar–39Ar dating of Eocene deformation in the Chiapas Fold and Thrust Belt, southern Mexico / Rogelio Hernández-Vergara, Elisa Fitz-Díaz, Gilles Brocard and Dante Jaime Morán-Zenteno / Geological Society, London, Special Publications, 504, 315-341, 11 September 2020, https://doi.org/10.1144/SP504-2020-75 --- Tectonic terranes underlying the present-day Caribbean plate: their tectonic origin, sedimentary thickness, subsidence histories and regional controls on hydrocarbon resources / Sean Romito and Paul Mann / Geological Society, London, Special Publications, 504, 343-377, 27 July 2020, https://doi.org/10.1144/SP504-2019-221 --- Integration of tectonic geomorphology and crustal structure across the active obliquely collisional zone on the island of Hispaniola, northeastern Caribbean / Lei Sun, Paul Mann and Dale E. Bird / Geological Society, London, Special Publications, 504, 379-400, 8 July 2020, https://doi.org/10.1144/SP504-2019-242 --- Regional hydrocarbon potential of the northeastern Caribbean based on integration of sediment thickness and source rock maturity data / Travis Tillman and Paul Mann / Geological Society, London, Special Publications, 504, 401-436, 16 November 2020, https://doi.org/10.1144/SP504-2019-244 --- Stratigraphy and structure of regionally-isolated hydrocarbon occurrences in the Azua Basin, south-central Dominican Republic (Northeastern Caribbean) / Paul Mann and Stephen Pierce / Geological Society, London, Special Publications, 504, 437-478, 16 November 2020, https://doi.org/10.1144/SP504-2019-241 --- New constraints on the tectonosedimentary evolution of the offshore San Pedro Basin (southeastern Dominican Republic): implications for its hydrocarbon potential / J. M. Gorosabel-Araus, J. L. Granja-Bruña, A. Gallego-Mingo, L. Gómez de la Peña, A. Rodríguez-Zurrunero, R. Mas, A. Carbó-Gorosabel and J. Navarro-Comet / Geological Society, London, Special Publications, 504, 479-505, 5 August 2020, https://doi.org/10.1144/SP504-2019-224 --- Cretaceous geology and tectonic assembly of Jamaica / Simon F. Mitchell / Geological Society, London, Special Publications, 504, 507-547, 2 September 2020, https://doi.org/10.1144/SP504-2019-210 --- Foldout maps --- The basins and orogens of the Southern Gulf of Mexico map / Ian Steel and Ian Davison / Geological Society, London, Special Publications, 504, 557-558, 14 December 2020, https://doi.org/10.1144/SP504-2020-2 --- Map of the geology of the Northern Caribbean and the Greater Antillean Arc / Ian Steel and Ian Davison / Geological Society, London, Special Publications, 504, 559-560, 14 December 2020, https://doi.org/10.1144/SP504-2020-3
    Pages: Online-Ressource (VIII, 556 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786204943
    Language: English
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  • 3
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 117 (1993), S. 327-335 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Chondrus crispus (Stackhouse) is a perennial red seaweed, common in intertidal and shallow sublittoral communities throughout the North Atlantic Ocean. In the intertidal zone, C. crispus may experience rapid temperature changes of 10 to 20C° during a single immerison-emerision cycle, and may be exposed to temperatures that exceed the thermal limits for long-term survival. C. crispus collected year-round at Long Cove Point, Chamberlain, Maine, USA, during 1989 and 1990, underwent phenotypic acclimation to growth temperature in the laboratory. This phenotypic acclimation enhanced its ability to withstand brief exposure to extreme temperature. Plants grown at summer seawater temperature (20°C) were able to maintain constant rates of lightsaturated photosynthesis at 30°C for 9 h. In contrast, light-saturated photosynthetic rates of plants grown at winter seawater temperature (5°C) declined rapidly following exposure to 30°C, reached 20 to 25% of initial values within 10 min, and then remained constant at this level for 9 h. The degree of inhibition of photosynthesis at 30°C was also dependent upon light intensity. Inhibition was greatest in plants exposed to 30°C in darkness or high light (600 μmol photons m-2s-1) than in plants maintained under moderate light levels (70 to 100 μmol photons m-2s-1). Photosynthesis of 20°C-acclimated plants was inhibited by exposure to 30°C in darkness or high light, but the degree of inhibition was less than that exhibited by 5°C-grown plants. Not only was light-saturated photosynthesis of 20°C plants less severely inhibited by exposure to 30°C than that of 5°C plants, but the former also recovered faster when they were returned to growth conditions. The mechanistic basis of this acclimation to growth temperature is not clear. Our results indicate that there were no differences between 5 and 20°C-grown plants in the thermal stability of respiration, electron transport associated with Photosystems I or II, Rubisco or energy transfer between the phycobilisomes and Photosystem II. Overall, our results suggest that phenotypic acclimation to seawater temperature allows plants to tolerate higher temperatures, and may play an important role in the success of C. crispus in the intertidal environment.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Corporate governance 2 (1994), S. 0 
    ISSN: 1467-8683
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Political Science , Economics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    The @journal of organic chemistry 55 (1990), S. 1432-1438 
    ISSN: 1520-6904
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 70 (1981), S. 842-849 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract A study of biotite cooling ages in the Adrar des Iforas Pan African belt has been made using Rb/Sr techniques. The results indicate that uplift of this segment of the belt probably took place soon after intrusion of the last granites in each particular area. Comparison of the cooling ages in all the Pan African belts suggest there is a bi-partite age division and thus a diachronism in the Pan African.
    Abstract: Résumé On a fait l'étude des âges de refroidissement des biotites dans la chaÎne panafricaine dans l'Adrar des Iforas suivant la technique Rb/Sr. Les résultats indiquent que le soulèvement de cette partie de la chaÎne eut lieu bientÔt après l'intrusion des derniers granites. La comparaison des âges de refroidissement dans toutes les chaÎnes panafricaines suggère qu'il y a une différence d'âge entre deux domaines et donc un diachronisme dans le Panafricain.
    Notes: Zusammenfassung Abkühlungsalter von Biotiten aus dem Adrar des Iforas im Panafrikanischen Gürtel wurden mit der Rb/Sr-Methode untersucht. Die Ergebnisse zeigen, da\ der Aufstieg dieses Abschnittes des Gürtels wahrscheinlich kurze Zeit nach der Intrusion der letzten Granite in jedem einzelnen Gebiet erfolgte. Der Vergleich von Abkühlungsaltern in allen Panafrikanischen Gürteln legt nahe, da\ es eine zweiteilige Altersgruppierung gibt und somit einen Diachronismus im Panafrikanischen Ereignis.
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  • 8
    ISSN: 1432-1939
    Keywords: Desiccation ; Fucoid ; Development ; Intertidal ecology ; Phaeophyta
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The effect of tidal emersion on survivorship, photosynthesis and embryonic development was studied in 8 h old zygotes and 7 d old embryos of the intertidal brown alga Pelvetia fastigiata (J. Ag.) DeToni. Zygotes and embryos were outplanted for single low tides in the intertidal zone on the central coast of California (U.S.A.) during June, 1990. Both zygotes and embryos exhibited close to 100% survival when outplanted beneath the canopy of adult P. fastigiata. Embryos (7 d old) also exhibited high survival when outplanted in a red algal turf, the microhabitat where most successful recruitment occurs. However, zygotes (8 h old) experienced high mortality (65–90%) when outplanted in the turf microhabitat. Embryos and zygotes that survived emersion experienced sub-lethal stress that temporarily impaired light-saturated photosynthesis when plants were reimmersed in seawater. The effects of sub-lethal stress were more pronounced in 8 h old zygotes than 7 d embryos, and more severe in the turf microhabitat than beneath the adult Pelvetia canopy. Zygotes outplanted in the red algal turf did not re-establish net photosynthesis until at least 6 h after re-immersion. Photosynthesis was less inhibited in 8 h old zygotes outplanted beneath the adult Pelvetia canopy, and recovered to control (non-emersed) levels within 3 h of re-immersion. Embryos (7 d old) were able to achieve positive net photosynthesis immediately on re-immersion after emersion in the turf or canopy microhabitats. Emersion also retarded the rate of embryonic development in 8 h old zygotes, delaying the formation of primary rhizoids, which help to attach the plant to the substrate. For example, at 19 h post-fertilization, 75% of control (non-emersed) zygotes had developed rhizoids, compared to 3% and 30% for zygotes outplanted in the turf and canopy microhabitats. The different emersion responses of 8 h old zygotes and 7 d old embryos appeared to be related to their ability to tolerate cellular dehydration. Overall, our data suggest that the effects of sub-lethal stresses may have been underestimated in studies of intertidal ecology.
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  • 9
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    In:  Geological Society Special Publication 272: 345-359.
    Publication Date: 2007-10-08
    Description: This paper first reviews the salt basins and depositional ages in the South Atlantic salt province. This comprises a series of salt basins separated by basement highs, deep graben (that never dried up), later volcanic highs and subaerial ocean spreading ridges. Initial halite and anhydrite deposition occurred first in the Sergipe-Alagoas Basin of NE Brazil at c. 124.8 Ma, and was closely followed by deposition in the Kwanza Basin, Angola between 124.5 and 121 Ma. The later potassium-magnesium-rich salts were deposited in the Sergipe-Alagoas and Gabon-Congo basins before 114.5 Ma. The age of the main Santos-Campos salt is not known precisely, but the latest anhydrites deposited on the southern margin of the Santos Basin post-date volcanic rocks dated at 113.2 Ma. The paper then compares the salt tectonics of the wide Campos-Santos Basin segment with the narrow South Bahia basins segment. Sediment loading in the Santos Basin produced a landward-dipping base salt, which led to the development of counter-regional faults, and inhibited downslope sliding, and enhanced later contractional effects caused by either gravity spreading or regional tectonic compression. Folding occurred in simultaneous pulses across the Santos Basin, suggesting that regional tectonic compression occurred. The narrow salt basins of South Bahia have a steeply dipping base salt horizon (4{degrees}) and pronounced folding, which initiates at the oceanward pinch-out of the salt and propagates back up the slope. The topographic highs, above fold anticlines, are rapidly eroded on narrow margin slopes, which allows the folds to grow more easily to large amplitudes at the top salt horizon.
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  • 10
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    In:  Geological Society Special Publication 363: 159-174.
    Publication Date: 2012-02-13
    Description: The southern Brazilian salt basin, comprising the three sub-basins Santos, Campos and Espirito Santo, was deposited over a pre-existing rifted basin with c. 1–2 km of relief bordered by an outer basin high that separated the basin from the conjugate African margin. The evaporites are interpreted to have been deposited very rapidly (〈1 Ma) during the waning of extension. Deposition of salt caused rapid loading of the basin, so that further basin subsidence occurred and mobile salt drained from structurally higher zones into the subsiding basins. Seismic evidence indicates that downslope salt drainage occurred before any sediment overburden accumulated. Withdrawal synclines within salt units developed adjacent to diapirs, which have intruded the evaporite sequence, and salt extrusions are observed which were buried by later salts. The early movement of the salt probably contributed to significant fault reactivation and redistribution of salt load, so that the final half-graben salt fill reached up to 4.5 km thick where only 1–2 km of salt was originally deposited.
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