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  • 1
    Monograph available for loan
    Monograph available for loan
    Geomagnetické pole : a jeho prínos k objasnení vývoje Zeme (1975)
    Praha : Academia
    Details Availability
    Call number: G 7076
    Type of Medium: Monograph available for loan
    Pages: 366 S. : graph. Darst.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Crustal structure of the Bohemian Massif and the West Carpathians : with 124 tables (1994)
    Berlin [u.a.] : Springer
    Details Availability
    Call number: 4/M 96.0354
    Type of Medium: Monograph available for loan
    Pages: xiii, 355 S.
    ISBN: 3540579869
    Series Statement: Exploration of the deep continental crust
    Classification:
    Tectonics
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
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    Geomagnetic forcing and climatic variations in Europe, North America and in the Pacific Ocean (2002)
    Elsevier
    Details
    Publication Date: 2002-05-01
    Print ISSN: 1040-6182
    Electronic ISSN: 1873-4553
    Topics: Geography , Geosciences
    Published by Elsevier
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    PAPER CURRENT
  • 4
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    Geomagnetic forcing of changes in climate and in the atmospheric circulation (1998)
    Elsevier
    Details
    Publication Date: 1998-01-01
    Print ISSN: 1364-6826
    Electronic ISSN: 1879-1824
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 5
    Electronic Resource
    Electronic Resource
    Changes of the Earth's Magnetic Moment and Radiocarbon Dating (1969)
    [s.l.] : Nature Publishing Group
    Nature 224 (1969), S. 681-683 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Three archaeomagnetic curves9'10?for Europe, Central America and Japans-provide convenient data for studying the westward drift (Fig. 1), because the territories from which these samples were taken are equally spaced around the globe (Europe 15 E, Central America 255 W, Japan 135 E). It is also ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/224681a0
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  • 6
    Electronic Resource
    Electronic Resource
    Paläomagnetische Komplexuntersuchungen an Eruptiv- und Sedimentgesteinen des Böhmischen Massivs (1965)
    Springer
    Pure and applied geophysics 61 (1965), S. 101-112 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Complex methods, used at Potsdam since 1960 [4, 5, 6]3), nowadays are successfully tried for paleomagnetic studies also. Results in this direction in the following are discussed in detail.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00875766
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  • 7
    Electronic Resource
    Electronic Resource
    Palaeomagnetism and continental drift (1975)
    Springer
    Studia geophysica et geodaetica 19 (1975), S. 300-305 
    Details
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary The pattern of palaeomagnetic curves with particular regard to the lower Palaeozoic epochs which was revised by a suitable choice of polarity of data for the individual continents is given. The investigated distribution of the continental blocks for the individual geological epochs agrees with all the palaeontological and geological facts. The comparison of the model of continental drift with the occurrence of orogenic events and some palaeontological conclusions was carried out.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01614261
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  • 8
    Electronic Resource
    Electronic Resource
    Remanent magnetism of anorganic and organic substances and its exploitation in treating historical problems (1971)
    Springer
    Studia geophysica et geodaetica 15 (1971), S. 353-363 
    Details
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary Properties of the thermoremanent magnetization of various archaeological materials (baked-clay objects, samples from old trees, bones and stones) were investigated with the purpose to assess the possibility of their use for the determination of the earth's magnetic field in the historical past and to apply the data for solving some practical problems. It turns out that most of those materials yield magnetic values that can be used for making the radiocarbon dating method more accurate, for determining the degree of burning and for direct archaeomagnetic dating. The new conclusions also contribute to the knowledge of changes in the earth's magnetic field in the past.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01589251
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  • 9
    Electronic Resource
    Electronic Resource
    The intensity of the earth's magnetic field in the past derived from the archaeomagnetic data (1972)
    Springer
    Studia geophysica et geodaetica 16 (1972), S. 407-410 
    Details
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Резюме Полученныŭ зa nосле¶rt;нuе о¶rt;ы фaкmuческuŭ мamерuaл об uзмененuu нanряженносmu еомa нumно о nоля зa nосле¶rt;нuе 8500 леm nозволяеm выявumь нauболее хaрaкmерные черmы в uзмененuu эmо о naрaмеmрa. Усре¶rt;ненuе мuровых ¶rt;aнных ¶rt;ля Ф в целом u ¶rt;ля оm¶rt;елъных mеррumорuŭ рaзлuчнымu сnособaмu nрuвелu к aнaло uчным резульmamaм [1–3] (Puc. 1.B). Сnекmрaльныŭ aнaлuз вaрuaцuŭ (Puc.2) оmсеnaрuровaнных оm основно о моноmонно о mрен¶rt;a, ¶rt;ля нauболее nо¶rt;робноŭ чaсmu крuвоŭ, оmносящеŭся к nосле¶rt;нuм 2-м mысячaм леm, оmчеmлuво nокaзaл нaлuчuе nерuо¶rt;ов nоря¶rt;кa 1000 леm u 350 леm, лежaщuх нa уровне знaчuмосmu, сооmвеmсmвующем 80%-ноŭ верояmносmu. Кaчесmвенное срaвненuе хо¶rt;a крuвых нanряженносmu ¶rt;ля оm¶rt;ельных mеррumорuŭ (конmuненmов) nокaзaло нaлuчuе uссле¶rt;уемо о эффекma u ¶rt;ля эmо о naрaмеmрa[5] (Puc. 3). Колuчесmвеннaя оценкa в резульmamе сnекmрaльно о aнaлuзa nокaзaлa нaлuчuе nерuо¶rt;ов nоря¶rt;кa 750 леm, 200 леm u менее вырaженныŭ — 300 леm. (Puc. 4.) По совокуnносmu мuровых ¶rt;aнных nосmроенa кaрmuнa рaсnре¶rt;еленuя nосле¶rt;нuх nо временu эксmремaльных mочек (мaксuмумов) в зaвuсuмосmu оm ¶rt;ол оmы месm (Puc. 5). Сaмaя больщaя mру¶rt;носmь nрu оценке naрaмеmров еомa нumно о nоля зaключaеmся в вы¶rt;еленuu вmорuчных колебaнuŭ, aмnлumу¶rt;a коmорых соuзмерuмa с nо рещносmью меmо¶rt;a.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01624172
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  • 10
    Electronic Resource
    Electronic Resource
    The continuous pattern of variations of the geomagnetic field in the quaternary and their causes (1973)
    Springer
    Studia geophysica et geodaetica 17 (1973), S. 218-231 
    Details
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary Apart from a brief account of the theories of the geomagnetic field and from suggestions of obtaining new data, the present work contains an analysis of the results of investigations into continental Quaternary sediments, which have become the object of close palaeomagnetic studies in Czechoslovakia in recent years. Besides sea sediments they represent one of the few possibilities of obtaining more complete data on the past of the geomagnetic field even though their investigation requires instruments of high sensitivity and exact processing technique. A brief geological description and chronological list of individual sedimentary cycles are presented and the results of their palaeomagnetic investigation on a number of samples (about 2 000) are given. The obtained results suggest that the geomagnetic field probably displayed successive changes in the position of its magnetic axis shifting from the region of the south pole to the region of the north pole over a period of approximately 2.5 millions of years in the form of oscillations caused by impulses recurring at periods of about 140 000 years. Three types of changes of the geomagnetic field with different periods can be identified (Fig. 2): not always expressive changes with the period of 2.5 × 10 4 years, quasisinusoidal changes with a period of about 1.4 × 10 5 years and long-term changes most likely also periodical with the period of about 2.5 × 10 6 years. The first and the second periods, particularly, are close to the precession constants as far as the magnitude is concerned. Thus it can be stated that the differences in the precession rates of the motion of the core and the mantle may markedly act together in the origin of the geomagnetic field.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01626584
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