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  • 1
    Monograph available for loan
    Monograph available for loan
    Collision and Collapse at the Africa-Arabia-Eurasia Subduction Zone (2009)
    London : The Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(311)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 368 S.
    ISBN: 9781862392700
    Series Statement: Geological Society special publication 311
    URL: http://sp.lyellcollection.org/content/vol311/issue1/
    Classification:
    Tectonics
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
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    Collision and Collapse at the Africa-Arabia-Eurasia Subduction Zone (2009)
    London : The Geological Society
    Details
    Description / Table of Contents: Geodynamics of collision and collapse at the Africa–Arabia–Eurasia subduction zone – an introduction / Douwe J. J. van Hinsbergen, Michael A. Edwards and Rob Govers / Geological Society, London, Special Publications, 311, 1-7, 29 April 2009, https://doi.org/10.1144/SP311.1 --- Melange genesis and ophiolite emplacement related to subduction of the northern margin of the Tauride–Anatolide continent, central and western Turkey / Alastair H. F. Robertson, Osman Parlak and Tı̇mur Ustaömer / Geological Society, London, Special Publications, 311, 9-66, 29 April 2009, https://doi.org/10.1144/SP311.2 --- Tectono-stratigraphy of the Çankırı Basin: Late Cretaceous to early Miocene evolution of the Neotethyan Suture Zone in Turkey / Nuretdin Kaymakci, Yakup Özçelik, Stanley H. White and Paul M. Van Dijk / Geological Society, London, Special Publications, 311, 67-106, 29 April 2009, https://doi.org/10.1144/SP311.3 --- Oligocene–Miocene basin evolution in SE Anatolia, Turkey: constraints on the closure of the eastern Tethys gateway / Silja K. Hüsing, Willem-Jan Zachariasse, Douwe J. J. van Hinsbergen, Wout Krijgsman, Murat Inceöz, Mathias Harzhauser, Oleg Mandic and Andreas Kroh / Geological Society, London, Special Publications, 311, 107-132, 29 April 2009, https://doi.org/10.1144/SP311.4 --- Long-term evolution of the North Anatolian Fault: new constraints from its eastern termination / Aurélia Hubert-Ferrari, Geoffrey King, Jérome van der Woerd, Igor Villa, Erhan Altunel and Rolando Armijo / Geological Society, London, Special Publications, 311, 133-154, 29 April 2009, https://doi.org/10.1144/SP311.5 --- Mediterranean snapshots of accelerated slab retreat: subduction instability in stalled continental collision / M. A. Edwards and B. Grasemann / Geological Society, London, Special Publications, 311, 155-192, 29 April 2009, https://doi.org/10.1144/SP311.6 --- Evolution of the southern Tyrrhenian slab tear and active tectonics along the western edge of the Tyrrhenian subducted slab / Andrea Argnani / Geological Society, London, Special Publications, 311, 193-212, 29 April 2009, https://doi.org/10.1144/SP311.7 --- Geochemical and temporal evolution of Cenozoic magmatism in western Turkey: mantle response to collision, slab break-off, and lithospheric tearing in an orogenic belt / Yildirim Dilek and Şafak Altunkaynak / Geological Society, London, Special Publications, 311, 213-233, 29 April 2009, https://doi.org/10.1144/SP311.8 --- Insights from the Apennines metamorphic complexes and their bearing on the kinematics evolution of the orogen / Gianluca Vignaroli, Claudio Faccenna, Federico Rossetti and Laurent Jolivet / Geological Society, London, Special Publications, 311, 235-256, 29 April 2009, https://doi.org/10.1144/SP311.9 --- Sequential development of interfering metamorphic core complexes: numerical experiments and comparison with the Cyclades, Greece / C. Tirel, P. Gautier, D. J. J. van Hinsbergen and M. J. R. Wortel / Geological Society, London, Special Publications, 311, 257-292, 29 April 2009, https://doi.org/10.1144/SP311.10 --- The Itea–Amfissa detachment: a pre-Corinth rift Miocene extensional structure in central Greece / Dimitrios Papanikolaou, Leonidas Gouliotis and Maria Triantaphyllou / Geological Society, London, Special Publications, 311, 293-310, 29 April 2009, https://doi.org/10.1144/SP311.11 --- Neogene brittle detachment faulting on Kos (E Greece): implications for a southern break-away fault of the Menderes metamorphic core complex (western Turkey) / Douwe J. J. van Hinsbergen and Flora Boekhout / Geological Society, London, Special Publications, 311, 311-320, 29 April 2009, https://doi.org/10.1144/SP311.12 --- Magnetostratigraphy of early–middle Miocene deposits from east–west trending Alaşehir and Büyük Menderes grabens in western Turkey, and its tectonic implications / Sevket Sen and Gürol Seyitoğlu / Geological Society, London, Special Publications, 311, 321-342, 29 April 2009, https://doi.org/10.1144/SP311.13 --- The structure of the Kythira–Antikythira strait, offshore SW Greece (35.7°–36.6°N) / Eleni Kokinou and Evangelos Kamberis / Geological Society, London, Special Publications, 311, 343-360, 29 April 2009, https://doi.org/10.1144/SP311.14 --- Erratum --- Melange genesis and ophiolite emplacement related to subduction of the northern margin of the Tauride–Anatolide continent, central and western Turkey / Alastair H. F. Robertson, Osman Parlak and Tı̇mur Ustaömer / Geological Society, London, Special Publications, 311, 1, 29 July 2009, https://doi.org/10.1144/SP311.Erratum
    Pages: Online-Ressource (368 Seiten)
    ISBN: 9781862392700
    URL: http://sp.lyellcollection.org/content/311/1
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Free amino acids and osmoregulation in penaeid shrimp (1975)
    s.l. : American Chemical Society
    Journal of agricultural and food chemistry 23 (1975), S. 1172-1174 
    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/jf60202a015
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    Paper (German National Licenses)
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  • 4
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    Extensional crustal-scale shear zones in the Western Cyclades (Kea, Greece) (2010)
    Universitätsverlag Göttingen
    Details
    Publication Date: 2021-03-29
    Description: Intense seismicity and intensely developed active and ancient fault systems are common to the Aegean Region. Extending/ thinning crust involves a complex interplay of (1) Gulf of Corinth riftexpansion, (2) west- and south-ward retreat of the Hellenic Trench, (3) westward impingement of the Anatolian Platen, and/or (4) propagation of the Anatolian Fault system into the Aegean. New geological/structural investigations on Kea (also known as Tzia), in the Western Cyclades reveal a low angle crustal-scale, detachment-type ductile shear zone probably formed during Miocene extension and thinning of the continental crust...
    Description: conference
    Keywords: 551 ; VEF 300 ; VAE 130 ; VKB 270 ; VAE 400 ; Griechenland und griechische Inseln {Geologie} ; Geomechanik ; Produkte mechanischer Deformation {Petrologie} ; Tektogenese {Geologie} ; Kea ; Erdkruste ; Extension 〈Geologie〉 ; Scherzone
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 5
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    The Serifos Metamorphic Core Complex (Greece) — kinematic investigations of the southern detachment mylonites (2010)
    Universitätsverlag Göttingen
    Details
    Publication Date: 2021-03-29
    Description: The island of Serifos is situated about 100km SSE of Athens in the Aegean Sea and belongs to the Attic-Cycladic massif. The geology of Serifos is largely characterized by a shallow hornblendebiotite granodiorite pluton that intruded in the late Miocene into a previously deformed (under blueschist conditions) sequence mainly consisting of ortho- and paragneisses, calc-silicate marbles, amphibolites and schists. The pluton has a dome-shaped body occupying the central and southern parts of the island (Salemink 1985). The Serifos MCC is the very western continuation of a zone of syn- to post tectonic intrusions younging from the East (Naxos, Paros ?12Ma) to the West (Serifos 9– 8Ma). Whereas the older intrusions in the East show a top to the North geometry, the Serifos MCC has developed a South-directed low-angle detachment fault...
    Description: conference
    Keywords: 551 ; VEF 300 ; VKB 292 ; VKB 270 ; VAE 140 ; Griechenland und griechische Inseln {Geologie} ; Metamorphe Komplexe, übriges Europa {Petrologie} ; Produkte mechanischer Deformation {Petrologie} ; Gesteinsdeformation {Strukturgeologie} ; Serifos ; Scherzone ; Mylonit ; Krustenbewegung
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 6
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    Kinematics and deformation structures in a crustal-scale shear zone on Kea (W. Cyclades, Greece) (2010)
    Universitätsverlag Göttingen
    Details
    Publication Date: 2021-03-29
    Description: It is generally agreed upon that the exhumation of metamorphic rocks in the Aegean is caused by post orogenic extension in the late Oligocene to early Miocene. This extension is in principle largely accommodated by low-angle crustal detachment faulting possibly resulting in the formation of metamorphic core complexes (MCC). Here, we present data from recent structural investigations on the island of Kea in the W. Cyclades, Greece. Our work focussed in the north of the island. Of the ca. 270m total structural thickness that was mapped, the entire section of rocks are highly strained. Exhumation during progressive deformation is recorded by the transition from ductile to brittle/ductile to brittle conditions. The regional characteristics and types of deformation structures vary depending on the protolith and the intensity of strain...
    Description: conference
    Keywords: 551 ; VAE 860 ; VAE 400 ; VAE 140 ; VEF 300 ; VKB 292 ; VKB 270 ; Festlandkerne {Geologie} ; Tektogenese {Geologie} ; Gesteinsdeformation {Strukturgeologie} ; Griechenland und griechische Inseln {Geologie} ; Metamorphe Komplexe, übriges Europa {Petrologie} ; Produkte mechanischer Deformation {Petrologie} ; Kea ; Scherzone ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 7
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    Rifting and strike-slip shear in central Tibet and the geometry, age and kinematics of upper crustal extension in Tibet (2011)
    In:  Geological Society Special Publication 353: 127-163.
    Details
    Publication Date: 2011-03-10
    Description: The youngest deformation structures on the Tibet Plateau are about NNE-trending grabens. We first combine remote-sensing structural and geomorphological studies with structural field observations and literature seismological data to study the Muga Purou rift that stretches at c. 86°E across central Tibet and highlight a complex deformation field. ENE-striking faults are dominated by sinistral strike–slip motion; NNE-striking faults have normal kinematics and outline a right-stepping en-echelon array of grabens, also suggesting sinistral strike–slip; along NW-striking fault sets, the arrangement of grabens may indicate a dextral strike–slip component. Thus, in central Tibet, rifts comprise mostly grabens connected to strike–slip fault zones or are arranged en-echelon to accommodate sinistral wrenching; overall strain geometry is constrictional, in which NNE–SSW and subvertical shortening is balanced by WNW–ESE extension. The overwhelmingly shallow earthquakes only locally outline active faults; clusters seem to trace linkage or propagation zones of know structures. The earthquake pattern, the neotectonic mapping, and the local fault–slip analyses emphasize a distributed, heterogeneous pattern of deformation within a developing regional structure and indicate that strain concentration is weak in the uppermost crust of central Tibet. Thus, the geometry of neotectonic deformation is different from that in southern Tibet. Next, we use structural and palaeomagnetic data along the Zagaya section of southern central Tibet to outline significant block rotation and sinistral strike–slip SE of the Muga Purou rift. Our analysis supports earlier interpretations of reactivation of the Bangong–Nujiang suture as a neotectonic strike–slip belt. Then, we review the existing and provide new geochronology on the onset of neotectonic deformation in Tibet and suggest that the currently active neotectonic deformation started c. 5 Ma ago. It was preceded by c. north–south shortening and c. east–west lengthening within a regime that comprises strike–slip and low-angle normal faults; these were active at c. 18–7 Ma. The c. east-striking, sinistral Damxung shear zone and the c. NE-trending Nyainqentanghla sinistral-normal detachment allow speculations about the nature of this deformation: the ductile, low-angle detachments may be part of or connect to a mid-crustal décollement layer in which the strike–slip zones root; they may be unrelated to crustal extension. Finally, we propose a kinematic model that traces neotectonic particle flow across Tibet and speculate on the origin of structural differences in southern and central Tibet. Particles accelerate and move eastwards from western Tibet. Flow lines first diverge as the plateau is widening. At c. 92°E, the flow lines start to converge and particles accelerate; this area is characterized by the appearance of the major though-going strike–slip faults of eastern-central Tibet. The flow lines turn southeastward and converge most between the Assam–Namche Barwa and Gongha syntaxes; here the particles reach their highest velocity. The flow lines diverge south of the cord between the syntaxes. This neotectonic kinematic pattern correlates well with the decade-long velocity field derived from GPS-geodesy. The difference between the structural geometries of the rifts in central and southern Tibet may be an effect of the basal shear associated with the subduction of the Indian plate. The boundary between the nearly pure extensional province of the southern Tibet and the strike–slip and normal faulting one of central Tibet runs obliquely across the Lhasa block. Published P-wave tomographic imaging showed that the distance over which Indian lithosphere has thrust under Tibet decreases from west to east; this suggests that the distinct spatial variation in the mantle structure along the collision zone is responsible for the surface distribution of rift structures in Tibet.Supplementary material: Containing supporting data is available at http://www.geolsoc.org.uk/SUP18446.
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  • 8
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    Geodynamics of collision and collapse at the Africa-Arabia-Eurasia subduction zone - an introduction (2009)
    In:  Geological Society Special Publication 311: 1-7.
    Details
    Publication Date: 2009-04-30
    Description: Shortly after the recognition of plate-tectonics, Wilson (1966) proposed his now famous cycle describing the creation and demise of ocean basins. His original four stages still form the basis for plate-tectonic discussions today: (1) rifting of a continent; (2) continental drift, sea-floor spreading and formation of ocean basins; (3) subduction initiation and progressive closure of ocean basins by subduction of oceanic lithosphere; and (4) continent–continent collision and final closure of an ocean basin. The Mediterranean basin constitutes the westernmost extremity of the Tethyan domain (e.g. Stampfli & Borel 2002). Here, the last remains of this former oceanic basin have nearly disappeared, thus representing stage (4). This final closure phase is associated with rifting and drifting in the Western Mediterranean (Dercourt et al. 1986), and with initiation of the Tyrrhenian–Calabrian and Alboran subduction zones, i.e. all of Wilson's phases are occurring concurrently. Imprints of previous Wilson stages are preserved in the geological record. Detailed geochemical and metamorphic-petrological study of ophiolites – on-land relics of oceanic crust in mountain belts – (Spadea & D'Antonio 2006; Barth et al. 2008), paleogeographic reconstructions (Hall & Spakman 2003), as well as numerical and analogue modeling experiments (Chemenda et al. 2001; Toth & Gurnis 1998) have revealed that initiation of oceanic subduction, as the first part of Wilson's phase 3, may start in various ways, e.g. by inversion of a mid-oceanic ridge or fracture zone, or subduction polarity reversal. The subsequent oceanic subduction stage closes...
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  • 9
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    Aldosterone-stimulating somatic gene mutations are common in normal adrenal glands (2015)
    National Academy of Sciences
    Details
    Publication Date: 2015-08-03
    Description: Primary aldosteronism (PA) represents the most common cause of secondary hypertension, but little is known regarding its adrenal cellular origins. Recently, aldosterone-producing cell clusters (APCCs) with high expression of aldosterone synthase (CYP11B2) were found in both normal and PA adrenal tissue. PA-causing aldosterone-producing adenomas (APAs) harbor mutations in genes encoding ion channels/pumps that alter intracellular calcium homeostasis and cause renin-independent aldosterone production through increased CYP11B2 expression. Herein, we hypothesized that APCCs have APA-related aldosterone-stimulating somatic gene mutations. APCCs were studied in 42 normal adrenals from kidney donors. To clarify APCC molecular characteristics, we used microarrays to compare the APCC transcriptome with conventional adrenocortical zones [zona glomerulosa (ZG), zona fasciculata, and zona reticularis]. The APCC transcriptome was most similar to ZG but with an enhanced capacity to produce aldosterone. To determine if APCCs harbored APA-related mutations, we performed targeted next generation sequencing of DNA from 23 APCCs and adjacent normal adrenal tissue isolated from both formalin-fixed, paraffin-embedded, and frozen tissues. Known aldosterone driver mutations were identified in 8 of 23 (35%) APCCs, including mutations in calcium channel, voltage-dependent, L-type, α1D-subunit (CACNA1D; 6 of 23 APCCs) and ATPase, Na+/K+transporting, α1-polypeptide (ATP1A1; 2 of 23 APCCs), which were not observed in the adjacent normal adrenal tissue. Overall, we show three major findings: (i) APCCs are common in normal adrenals, (ii) APCCs harbor somatic mutations known to cause excess aldosterone production, and (iii) the mutation spectrum of aldosterone-driving mutations is different in APCCs from that seen in APA. These results provide molecular support for APCC as a precursor of PA.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
    Published by National Academy of Sciences
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  • 10
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    Infrastructure to enable deployment of carbon capture, utilization, and storage in the United States [Sustainability Science] (2018)
    National Academy of Sciences
    Details
    Publication Date: 2018-09-19
    Description: In February 2018, the United States enacted significant financial incentives for carbon capture, utilization, and storage (CCUS) that will make capture from the lowest-capture-cost sources economically viable. The largest existing low-capture-cost opportunity is from ethanol fermentation at biorefineries in the Midwest. An impediment to deployment of carbon capture at ethanol...
    Keywords: Sustainability Science
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
    Published by National Academy of Sciences
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