Die Vereisung des Lilliehöökfjordes (Spitzbergen) in den Jahren 1941/42 und 1942/43     

Nusser  Franz 《Ocean Dynamics》1950,3(5-6):286-293

Ocean Dynamics - Die Eisbeobachtungen, die während der Überwinterungen 1941/42 und 1942/43 in dem Lilliehöökfjord gemacht wurden, werden mitgeteilt und daraus der Ablauf der...  相似文献   

Die Eisverhältnisse des Winters 1948/49 an den deutschen Küsten     

Franz Nusser 《Ocean Dynamics》1949,2(6):251-255

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猿,巨人及人     

魏敦瑞  刘东生 《地质论评》1949,14(Z1):75-79

全书共分五章,每章专论一题目,各自独立,但其总旨仍互相连贯。第一章人及其猿猴类之祖先此章由解剖学各方面证明在分类学上人与人猿最为相近,因其相差之程度,远较人猿与其他低等猿类为小。而在研究人类演化之过程  相似文献   

Zur Deutung der Vertikalbewegungen der Festländer und Meere     

Franz E. Sueß 《International Journal of Earth Sciences》1921,11(7-8):361-406

Ohne Zusammenfassung  相似文献   

III. Das Gebirge östlich von den Radstädter Tauern und vom Katschberg     

Dr. Franz Heritsch 《International Journal of Earth Sciences》1912,3(4):245-258

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Fortschritte in der geologischen Kenntnis der Zentralalpen westlich vom Brenner     

Dr. Franz Heritsch 《International Journal of Earth Sciences》1912,3(8):557-572

Ohne Zusammenfassung  相似文献   

Begriff und Bedeutung der Intrusionstektonik     

Franz Ed. Suess 《International Journal of Earth Sciences》1927,18(2):149-154

Ohne Zusammenfassung  相似文献   

Caledonian high-pressure metamorphism in the Strona-Ceneri Zone (Southern Alps of southern Switzerland and northern Italy)   总被引：3，自引：0，他引：3  

Leander Franz  Rolf L. Romer 《Swiss Journal of Geoscience》2007,100(3):457-467

The Strona-Ceneri Zone comprises a succession of polymetamorphic, pre-Alpidic basement rocks including ortho- and paragneisses, metasedimentary schists, amphibolites, and eclogites. The rock pile represents a Late Proterozoic or Palaeozoic subduction accretion complex that was intruded by Ordovician granitoids. Eclogites, which occur as lenses within the ortho-paragneiss succession and as xenoliths within the granitoids record a subduction related high-pressure event (D1) with peak metamorphic conditions of 710 ± 30 °C at 21.0 ± 2.5 kbar. After isothermal uplift, the eclogites experienced a Barrowtype (D2) tectonometamorphic overprint under amphibolite facies conditions (570-630 °C, 7-9 kbar). U-Pb dating on zircon of the eclogites gives a metamorphic age of 457 ± 5 Ma, and syn-eclogite facies rutile gives a ²⁰⁶Pb/²³⁸U age of 443 ± 19 Ma classifying the subduction as a Caledonian event. These data show that the main tectonometamorphic evolution of the Strona-Ceneri Zone most probably took place in a convergent margin scenario, in which accretion, eclogitization of MOR-basalt, polyphase (D1 and D2) deformation, anatexis and magmatism all occurred during the Ordovician. Caledonian high-pressure metamorphism, subsequent magmatism and Barrow-type metamorphism are believed to be related to subduction and collision within the northern margin of Gondwana. Editorial handling: Edwin Gnos  相似文献   

Investigation of a Tertiary maar structure using three-dimensional resistivity imaging   总被引：1，自引：0，他引：1  

Ingolf Brunner  Sven Friedel  Franz Jacobs  & Erik Danckwardt 《Geophysical Journal International》1999,136(3):771-780

This paper presents the application of the electrical resistivity tomography (ERT) method to the investigation of the Tertiary maar structure of Baruth (Germany) known from previous gravimetric surveys. ERT was applied to support the optimum location for a palaeoclimatological drill hole.
  Special modifications of data acquisition, signal processing and inversion are introduced to adapt the method of ERT to the special requirements for the 3-D investigation of structures with horizontal extensions of 1  km or more. More than 5000 dipole–dipole combinations were recorded at three concentric circular electrode arrangements using stand-alone transient data acquisition systems (RefTek).
  We present a fast approximate imaging technique based on the simultaneous iterative reconstruction technique (SIRT). As the complete calculation of the inverse Frechét matrix is avoided, the algorithm is especially suitable for large data and model spaces, where complete inversion is beyond the limits of available computing hardware. The single-step method is applicable to arbitrary irregular electrode layouts. Synthetic tests show that the imaging procedure reconstructs the main features of the subsurface.
  A low-resistivity body could be interpreted as limnic sediments filling the interior of the Tertiary maar crater. Considering the horizontal resistivity gradient, estimates for the lateral and depth extents of the structure were made. An optimum position for a palaeoclimatological borehole was found, and was in good agreement with the gravimetric minimum.  相似文献   

Spatial Distribution of Shelf- and Slope-Dwelling Fishes Collected by Bottom Longline off Lanzarote and Fuerteventura, Canary Islands     

Franz  Uiblein  Fernando  Bordes  Ricardo  Castillo Antonio G.  Ramos 《Marine Ecology》1998,19(1):53-66

Abstract. A total of 1789 fish belonging to 38 families and 73 species were collected at depths between 18 and 1102 m during 216 bottom longline operations off Lanzarote and Fuerteventura, Canary Islands, between February 1994 and December 1995. For each species the depth distribution is provided. Length-weight and depth-size relationships are reported for three shelf-dwelling species. The bigger-deeper relationship found in two of them contrasts with the bigger-shallower pattern of the deeper living trichiurid Lepidopus caudatus . In November 1997, nine additional bottom longline operations were carried out off eastern Fuerteventura at depths between 805 and 1217 m. In this area, after earlier studies in October 1995, a spawning aggregation of the morid Mora moro was encountered for the second time. The catches of 1997 revealed a strongly male-biased sex ratio. Also, the males showed a significantly lower gonadosomal index than two years earlier. These findings indicate slight interannual variations in reproductive timing and an earlier arrival of male Mora moro at the spawning grounds. Clear variations in the number of fish collected at adjacent sites possibly reflect a preference for distinct microhabitats. Preliminary evidence of local upwelling of cold water above the spawning grounds is provided by satellite imagery.  相似文献