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  • 1
    Electronic Resource
    Electronic Resource
    A human embryo of 28 mm crown-rump length with cerebral, esophagotracheal and cardiovascular malformations (1976)
    Springer
    Anatomy and embryology 150 (1976), S. 53-62 
    Details
    ISSN: 1432-0568
    Keywords: Human teratology ; Anophthalmia ; Cebocephalia ; Tracheoesophageal malformations ; Cardiovascular malformations
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary The following malformations were observed in a human embryo of 28 mm crown-rump length obtained at operation for tubal rupture in a case of extrauterine pregnancy: 1. Secondary anophthalmia with dysplasia and in part aplasia of the diencephalon. Rudiments of both eyes and eyestalklike proliferations within the diencephalon. No lenses and on the left side only a palpebral fissure. Hypoplasia of the right telencephalic hemisphere and of the right side of diencephalon, mesencephalon and proximal parts of the medulla oblongata. Pseudotumorous proliferations in the diencephalon, in the alar plate of the medulla oblongata (protruding into the fourth ventricle) and in the arachnoid. Hypoplasia of the right internal, middle, and external ear. Dysplasia and in part aplasia of facial osseous elements (cebocephalia). 2. Proximal esophageal atresia with distal tracheoesophageal fistula. 3. A Fallot's tetralogy with right-sided aortic arch and regressive right-sided ductus arteriosus, tricuspid atresia, hypoplasia of the right ventricle with excessive hypertrophy of its wall, and hypoplasia of the pulmonary trunk. Single left superior vena cava and abnormal, semicircular course of the stems of both coronary arteries.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00346286
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  • 2
    Electronic Resource
    Electronic Resource
    Haemorrhages in spinal cord with syringomyelia in a patient with haemophilia (1963)
    Springer
    Acta neuropathologica 2 (1963), S. 306-308 
    Details
    ISSN: 1432-0533
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Résumé Un jeune homme de 21-ans atteint d'hémophilie non héréditaire (manque du facteur anti-haemophilique) tombait malade d'un rhume vulgaire avec complaints de douleur cervicale. Après 3 jours il se développait une paraplégie. Examinations neurologiques, roentgenologiques et la biopsie de neurochirurgien démonstraient l'existence d'une hématomyélie. L'anatomie-pathologique fournait l'évidence d'une hémorragie massive très récente, d'hémorragies anciennes avec accumulation de pigment de fer et d'une cavitation dans le centre de la moëlle épinière avec formation de tissu glial (comparer avec une formation neurofibromateuse). Coincidence rare d'une hématomyélie et d'une syringomyélie.
    Notes: Summary A 21-year-old man, with non-hereditary haemophilia on the basis of a deficiency of anti-haemophilic factor, was affected by a banale infection accompanied by cervical pain, which three days later progressed to a paraplegia. Neurological, roentgenological and neurosurgical findings showed that there was a haematomyelia. Anatomical examination showed in addition to the recent massive haemorrhages, iron pigment, cavitation extending over the entire length of the spinal cord, and new tissue formation such as is considered to be characteristic of syringomyelia.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00686425
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  • 3
    Electronic Resource
    Electronic Resource
    Congenital cavities of the posterior fossa (1966)
    Springer
    Acta neuropathologica 6 (1966), S. 117-126 
    Details
    ISSN: 1432-0533
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Zusammenfassung Zwei dem Recessus lateralis anliegende, mit diesem jedoch nicht verbundene Cysten werden beschrieben. Die erste fand sich autoptisch bei einer psychiatrischen Patientin von 54 Jahren, die an einem cerebrovasculären Zwischenfall starb. Im zweiten Fall, einem 61 jährigen Mann, hatte der Neurochirung bei bilateraler Trepanation wegen eines akuten Hydrocephalus eine Cyste der rechten Kleinhirntonsille gefunden. Der Verfasser vermutet, daß in diesen Fällen Teile der ursprünglichen Flügelplatte ventrolateral vom Kleinhirn persistierten. Die erstmals vonKramer beschriebenen Cysten wurden ebenso dieser Anlage zugeschrieben. In Verbindung mit diesen Beobachtungen werden einige andere abnorme Höhlen und merkwürdige Defekte des Kleinhirns beschrieben.
    Notes: Summary Two cysts adjacent to the recessus lateralis, but without any connection with the latter, are described. The first was found at the autopsy of a female psychiatric patient of 54 years, who had died of a cerebrovascular accident. The second case, was that of a man 61 years old. The neurosurgeon, after performing bilateral trephination for an acute hydrocephalus had found, a cyst of the right tonsil of the cerebellum. The author supposes that in these cases parts of the original roof-plate had persisted latero-ventrally to the cerebellum. The cysts first described byKramer were also thought to originate from this tissue. Some other abnormal cavities and curious cerebellar defects are described in connection with these two cases.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00686757
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  • 4
    Electronic Resource
    Electronic Resource
    STRESS WAVE VELOCITY AND CRACK SYSTEM OF A MEDIUM (1974)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 22 (1974), S. 0 
    Details
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Two in situ measurements of stress wave velocity in a granodiorite massif were made. Firstly, the velocities close to the source were investigated (for elimination of the influence of cracks), and secondly, the velocities in different horizontal directions over a large area were studied from the viewpoint of their dependence on the crack system of the medium. A correlation between the mutual orientation of the cracks and the maximum or minimum values of the stress wave velocities was obtained.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2478.1974.tb00112.x
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  • 5
    Electronic Resource
    Electronic Resource
    Geochronological constraints on the timing of granitoid magmatism, metamorphism and post-metamorphic cooling in the Hercynian crustal cross-section of Calabria (2000)
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 18 (2000), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Exposed cross-sections of the continental crust are a unique geological situation for crustal evolution studies, providing the possibility of deciphering the time relationships between magmatic and metamorphic events at all levels of the crust. In the cross-section of southern and northern Calabria, U–Pb, Rb–Sr and K–Ar mineral ages of granulite facies metapelitic migmatites, peraluminous granites and amphibolite facies upper crustal gneisses provide constraints on the late-Hercynian peak metamorphism and granitoid magmatism as well as on the post-metamorphic cooling. Monazite from upper crustal amphibolite facies paragneisses from southern Calabria yields similar U–Pb ages (295–293±4 Ma) to those of granulite facies metamorphism in the lower crust and of intrusions of calcalkaline and metaluminous granitoids in the middle crust (300±10 Ma). Monazite and xenotime from peraluminous granites in the middle to upper crust of the same crustal section provide slightly older intrusion ages of 303–302±0.6 Ma. Zircon from a mafic to intermediate sill in the lower crust yields a lower concordia intercept age of 290±2 Ma, which may be interpreted as the minimum age for metamorphism or intrusion. U–Pb monazite ages from granulite facies migmatites and peraluminous granites of the lower and middle crust from northern Calabria (Sila) also point to a near-synchronism of peak metamorphism and intrusion at 304–300±0.4 Ma. At the end of the granulite facies metamorphism, the lower crustal rocks were uplifted into mid-crustal levels (10–15 km) followed by nearly isobaric slow cooling (c. 3 °C Ma−1) as indicated by muscovite and biotite K–Ar and Rb–Sr data between 210±4 and 123±1 Ma. The thermal history is therefore similar to that of the lower crust of southern Calabria. In combination with previous petrological studies addressing metamorphic textures and P–T  conditions of rocks from all crustal levels, the new geochronological results are used to suggest that the thermal evolution and heat distribution in the Calabrian crust were mainly controlled by advective heat input through magmatic intrusions into all crustal levels during the late-Hercynian orogeny.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1525-1314.2000.00267.x
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  • 6
    Electronic Resource
    Electronic Resource
    High-pressure granulite facies metamorphism in the Pan-African belt of eastern Tanzania: P–T–t evidence against granulite formation by continent collision (1998)
    Oxford, UK : Blackwell Science Ltd.
    Journal of metamorphic geology 16 (1998), S. 0 
    Details
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: To constrain the tectonic history of the Pan-African belt in Tanzania, we have studied the P–T  evolution of granulites from northern and eastern Tanzania representative for a large part of the southern Pan-African belt of East Africa (e.g. Pare, Usambara, Ukaguru and Uluguru Mountains). Thermobarometry (conventional and multireaction equilibria) on enderbites and metapelites gives 9.5–11 kbar and 810±40 °C during peak metamorphism at 650–620 Ma. This is consistent with the occurrence of both sillimanite and kyanite in metapelites and of the high-P granulite facies assemblage garnet–clinopyroxene–quartz in mafic rocks. Peak metamorphic conditions are surprisingly similar over a very large area with N-S and E-W extents of about 700 and 200 km respectively. The prograde metamorphic evolution in the entire area started in the kyanite field but evolved mainly within the sillimanite stability field. The retrograde P–T  evolution is characterized by late-stage kyanite in metapelites and garnet–clinopyroxene coronas around orthopyroxene in meta-igneous rocks. This is in agreement with thermobarometric results and isotopic dating, indicating a period of nearly isobaric and slow cooling prior to tectonic uplift. The anticlockwise P–T  path could have resulted from magmatic underplating and loading of the lower continental crust which caused heating and thickening of the crust. Substantial postmetamorphic crustal thickening of yet unknown age (presumably after 550 Ma) led subsequently to the exhumation of high-P granulites over a large area. The results are consistent with formation of the Pan-African granulites at an active continental margin where tonalitic intrusions caused crustal growth and heating 70–100 Ma prior to continental collision. The P–T–t path contradicts recent geodynamic models which proposed tectonic crustal thickening due to continental collision between East and West Gondwana as the cause of granulite formation in the southern part of the Pan-African belt.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1525-1314.1998.00150.x
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  • 7
    Electronic Resource
    Electronic Resource
    A model of velocity structure beneath Calabria, southern Italy, based on laboratory data
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 87 (1988), S. 325-337 
    Details
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0012-821X(88)90020-9
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  • 8
    Electronic Resource
    Electronic Resource
    Synchronous uplift of the lower crust of the Ivrea Zone and of Southern Calabria and its possible consequences for the Hercynian orogeny in Southern Europe
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 56 (1981), S. 305-320 
    Details
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0012-821X(81)90136-9
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  • 9
    Electronic Resource
    Electronic Resource
    Amplitude-frequency distribution of strong ground motion
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 38 (1985), S. 144-161 
    Details
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0031-9201(85)90152-9
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  • 10
    Electronic Resource
    Electronic Resource
    Preface
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 38 (1985), S. iii 
    Details
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0031-9201(85)90146-3
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