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  • Amphibolites  (2)
  • Deformation  (2)
  • Soil reclamation  (2)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 29 (1999), S. 434-436 
    ISSN: 1432-0789
    Keywords: Key words Carbon-13 ; nitrogen-15 tracers ; Soil labelling ; Soil organic matter ; Soil reclamation ; Wildfires
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  The restoration of the C and N cycles in the soil-plant system is a basic step for the reclamation of burnt soils. To evaluate accurately the efficacy of restoration techniques, it is necessary to use isotopic tracers and, therefore, a 13C-, 15N-labelled burnt soil should be made available. The present paper describes a technique for obtaining a 13C-, 15N-labelled burnt soil by burning a labelled forest soil in the laboratory.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 32 (2000), S. 494-499 
    ISSN: 1432-0789
    Keywords: Keywords Heated soils ; Nitrogen-15 ; Poultry manure ; Soil reclamation ; Wildfire
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  Poultry manure (PM) efficacy to improve burnt soil revegetation was evaluated to determine the lowest effective and the optimum dose for burnt soil reclamation. A 15N-labelled forest soil (LS) was used to set up six treatments: LS, laboratory burnt LS (BLS) and BLS with PM dose equivalent to 1 (BLS+PM1), 2 (BLS+PM2), 4 (BLS+PM4) and 8 Mg dry PM ha–1 (BLS+PM8). Ryegrass was sown in all treatments and grown for 3 months in a greenhouse. At harvesting, in the BLS treatment: (1) ryegrass yield was very low and the shoot:root ratio was high; (2) ryegrass-N content was closer to that of metabolic tissues or young plants than to structural tissues or mature plants; (3) most of the available endogenous N still remained in the soil inorganic N pool. These results suggested that, although seed germinated normally, ryegrass growth was stopped at an early developmental stage, producing small and weak plants unable to protect the burnt soil against erosion and to exploit the post-fire pulse of available N which, consequently, could be lost. The addition of PM to BLS increased the ryegrass yield from the lowest dose (BLS≈LS〈BLS+PM1〈 BLS+PM2〈BLS+PM4〈BLS+PM8;P〈0.05), the increase of the phytomass yield per Mg of added PM varying as follows: PM8〈PM1≤PM4〈PM2. The uptake of soil-available N by the ryegrass was greatly enhanced in all manured treatments, but the contribution of PM-N to plant nutrition was only significant in BLS+PM4 and BLS+PM8 treatments. The lowest effective PM dose was PM1 and the optimum cost-to-benefit ratio treatments were PM2 and PM4.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1437-3262
    Keywords: Triple junctions ; Aracena metamorphic belt ; Inverted metamorphic gradient ; Amphibolites ; Granulites ; Hercynian belt
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract New data on the petrology and structure of the Aracena metamorphic belt shows that this is a subduction-related, low-pressure/high-temperature complex developed by plate convergence at the north margin of Gondwana during the Paleozoic. The low-pressure, inverted metamorphic gradient in MORB-derived amphibolites resulted from heating from the continental hanging wall during subduction. This implies that the previous heating of the continental rocks was related to subduction of an oceanic ridge and the creation of a slab window beneath the continental margin. This slab window brought the asthenosphere in contact with the continental margin inducing a shallow thermal anomaly and partial melting of the lithospheric mantle resulting in boninite magmatism.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1437-3262
    Keywords: Magma mixing ; Granite ; Enclaves ; Iberian Massif ; Deformation ; Conduit ; Magma flow
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Gil-Marquez Complex is an exceptional outcrop of plutonic rocks ranging in composition from diorites to granites emplaced into Devonian terrigenous metasediments of the southernmost part of the Hercynian basement of Iberia. A combined study of this complex, including field geology, petrology, structural geology and geochemistry, reveals that it represents an ancient conduit of magma transport through the continental crust. This conduit allowed the intrusion of magmas of contrasted compositions. Two end-members and several hybrids are identified. The first end-member is a biotite granite and the second is a basaltic magma generated by partial melting of a depletedmantle source. Both magmas rose through a common channel in which favorable conditions for unstable flow and magma mixing occurred. The observed relations in the Gil-Márquez Complex show that mixing in conduits may be an important mechanism for producing homogeneous hybrid magmas.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 0016-7835
    Keywords: Key words Magma mixing ; Granite ; Enclaves ; Iberian Massif ; Deformation ; Conduit ; Magma flow
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The Gil-Márquez Complex is an exceptional outcrop of plutonic rocks ranging in composition from diorites to granites emplaced into Devonian terrigenous metasediments of the southernmost part of the Hercynian basement of Iberia. A combined study of this complex, including field geology, petrology, structural geology and geochemistry, reveals that it represents an ancient conduit of magma transport through the continental crust. This conduit allowed the intrusion of magmas of contrasted compositions. Two end-members and several hybrids are identified. The first end-member is a biotite granite and the second is a basaltic magma generated by partial melting of a depleted-mantle source. Both magmas rose through a common channel in which favorable conditions for unstable flow and magma mixing occurred. The observed relations in the Gil-Márquez Complex show that mixing in conduits may be an important mechanism for producing homogeneous hybrid magmas.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 0016-7835
    Keywords: Key words Triple junctions ; Aracena metamorphic belt ; Inverted metamorphic gradient ; Amphibolites ; Granulites ; Hercynian belt
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  New data on the petrology and structure of the Aracena metamorphic belt shows that this is a subduction-related, low-pressure/high-temperature complex developed by plate convergence at the north margin of Gondwana during the Paleozoic. The low-pressure, inverted metamorphic gradient in MORB-derived amphibolites resulted from heating from the continental hanging wall during subduction. This implies that the previous heating of the continental rocks was related to subduction of an oceanic ridge and the creation of a slab window beneath the continental margin. This slab window brought the asthenosphere in contact with the continental margin inducing a shallow thermal anomaly and partial melting of the lithospheric mantle resulting in boninite magmatism.
    Type of Medium: Electronic Resource
    Library Location Call Number Volume/Issue/Year Availability
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