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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Petrology. ; Mineralogy. ; Geology. ; Petrology. ; Mineralogy. ; Geology.
    Description / Table of Contents: 1 Introduction to Metamorphic Rocks, Rock Metamorphism, and Metamorphic Processes -- Metamorphic Rocks -- 3 Metamorphic Processes -- 4 Metamorphic Grade, conditions of metamorphism -- 5 Metamorphism of Ultramafic Rocks -- 6 Metamorphism of Dolomites and Limestones -- 7 Metamorphism of Pelitic Rocks (Metapelites) -- 8 Metamorphism of Marls, Marlstones (Marlites) -- 9 Metamorphism of Mafic Rocks -- 10 Metamorphism of Quartzofeldspatic Rocks.
    Abstract: This new edition of the classic textbook presents a large number of diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given set of metamorphic rocks may have formed. Other parameters that control metamorphic mineral assemblages are also discussed and pitfalls resulting from simplifications and generalizations are highlighted. The book discusses the most common metamorphic rock types, their nomenclature, structure and graphical representation of their mineral assemblages. Part I defines basic principles of metamorphism, introduces metamorphic processes, geologic thermometry and barometry and defines metamorphic grade. Part II presents in a systematic way mineralogical changes and assemblages found in the most common types of metamorphic rocks. The computation of diagrams is based on recent advances in quantitative petrology and geochemistry. An extensive bibliography, including the key contributions and classic papers in the field, make it an invaluable source book for graduate students and professional geologists.
    Type of Medium: Online Resource
    Pages: XVI, 467 p. 217 illus., 122 illus. in color. , online resource.
    Edition: 9th ed. 2023.
    ISBN: 9783031125959
    Series Statement: Springer Textbooks in Earth Sciences, Geography and Environment,
    DDC: 552
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing :
    Keywords: Environment. ; Renewable energy sources. ; Electric power production. ; Environmental Sciences. ; Renewable Energy. ; Electrical Power Engineering. ; Mechanical Power Engineering.
    Description / Table of Contents: Chapter 1: Thermal Structure of The Earth -- Chapter 2: History of Geothermal Energy Use -- Chapter 3: Geothermal Energy Resources -- Chapter 4: Uses of Geothermal Energy -- Chapter 5: Geothermal Potential Perspectives Final -- Chapter 6: Geothermal Probes Final -- Chapter 7: Groundwater Wells -- Chapter 8: Hydrothermal Systems -- Chapter 9: EGS -- Chapter 10: High-Enthalpy Geothermal Systems -- Chapter 11: Environmental Issues -- Chapter 12: Drilling Techniques -- Chapter 13: Geophysical Methods -- Chapter 14: Hydraulic Tests -- Chapter 15: Hydrochemistry -- Chapter 16: References.
    Abstract: The internal heat of the planet Earth represents an inexhaustible reservoir of thermal energy known as Geothermal Energy. The 2nd edition of the book covers the geologic and technical aspects of developing all forms of currently available systems using this "renewable" green energy. The book presents the distribution and transport of thermal energy in the Earth. Geothermal Energy is a base load energy available at all times independent of climate and weather. The text treats the efficiency of diverse shallow near surface installations and deep geothermal systems including hydrothermal and petrothermal techniques and power plants in volcanic high-enthalpy fields. The book also discusses environmental aspects of utilizing different forms of geothermal energy, including induced seismicity, noise pollution and gas release to the atmosphere. Chapters on hydraulic well tests, chemistry of deep hot water, scale formation and corrosion, development of geothermal probes, well drilling techniques and geophysical exploration complete the text. This book, for the first time, covers the full range of utilization of Geothermal Energy.
    Type of Medium: Online Resource
    Pages: X, 390 p. 181 illus., 158 illus. in color. , online resource.
    Edition: 2nd ed. 2021.
    ISBN: 9783030716851
    DDC: 333.7
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 15/M 12.0238
    Description / Table of Contents: Contents: Thermisches Regime der Erde.- Geschichte geothermischer Energienutzung.- Geothermische Energie-Ressourcen.- Geothermische Nutzungsmöglichkeiten.- Potentiale und Perspektiven geothermischer Energienutzung.- Erdwärmesonden.- Geothermische Brunnenanlagen.- Hydrothermale Nutzung, geothermische Dublette.- Enhanced-Geothermal-Systems (EGS), Hot-Dry-Rock Systeme (HDR), Deep-Heat-Mining (DHM).- Potentielle Umweltauswirkungen bei der tiefen Geothermie.- Bohrtechnik für Tiefbohrungen.- Geophysikalische Untersuchungen.- Hydraulische Untersuchungen, Tests.- Hydrothermische Untersuchungen.
    Type of Medium: Monograph available for loan
    Pages: IX, 287 S.
    ISBN: 9783642243301
    Classification:
    Geothermal Energy
    Location: Reading room
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 11/M 13.0253
    Description / Table of Contents: Petrogenesis of Metamorphic Rocks presents a large number of diagrams showing the stability relations among minerals and groups of minerals found in metamorphic rocks. The diagrams help to determine the pressure and temperature conditions under which a given set of metamorphic rocks may have formed. Other parameters that control metamorphic mineral assemblages are also discussed and pitfalls resulting from simplifications and generalizations are highlighted. The book discusses the most common metamorphic rock types, their nomenclature, structure and graphical representation of their mineral assemblages. Part I defines basic principles of metamorphism, introduces metamorphic processes, geologic thermometry and barometry and defines metamorphic grade. Part II presents in a systematic way mineralogical changes and assemblages found in the most common types of metamorphic rocks. The computation of diagrams is based on recent advances in quantitative petrology and geochemistry. An extensive bibliography, including the key contributions and classic papers in the field, make it an invaluable source book for graduate students and professional geologists.
    Type of Medium: Monograph available for loan
    Pages: XII, 428 S. : z. T. farb. Ill., graph. Darst.
    Edition: 8th ed.
    ISBN: 9783540741688
    Classification:
    Petrology, Petrography
    Former Title: Bis 5. Aufl. u.d.T. ---〉 Winkler, Helmut Gustav Franz: Petrogenesis of metamorphic rocks
    Location: Reading room
    Branch Library: GFZ Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 94.0419
    Type of Medium: Monograph available for loan
    Pages: XIV, 318 S.
    Edition: 6th ed., complete revision of Winkler`s textbook
    ISBN: 3540575677
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 94.0522 ; AWI G1-96-0116
    Type of Medium: Monograph available for loan
    Pages: XIV, 318 S.
    Edition: 6th ed., complete rev. of Winkler's textbook
    ISBN: 3540575677
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 7
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 10/M 04.0469
    Type of Medium: Monograph available for loan
    Pages: XV, 341 S. , graph. Darst.
    Edition: 7th, completely rev. and updated ed.
    ISBN: 3540431306
    Classification:
    Petrology, Petrography
    Location: Reading room
    Branch Library: GFZ Library
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  • 8
    Call number: M 222
    Type of Medium: Monograph available for loan
    Pages: 251 S. : Ill., graph. Darst., Tab.
    Note: Zürich, Eidgenöss. Techn. Hochsch., Diss., 1977
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 9
    Publication Date: 2023-06-17
    Description: The composition of meta-gabbro and meta-basalt occurring abundant and widespread in all nappes of the nappe stack exposed in the Zermatt region of the Western Alp shows distinct patterns related to the geodynamic origin of metamorphic basic rocks. Eclogitic meta-basalts of the ophiolitic Zermatt-Saas Unit (ZSU) show enriched MORB signatures. The meta-basalts (eclogites) of the continental fragment of the Theodul Glacier Unit (TGU) derive from pre-Alpine metamorphic continental intraplate basalts. Meta-basalts (eclogites) from the continental basement of the Siviez-Mischabel nappe (SMN) derive from MORB thus a genetic relation to the TGU eclogites can be excluded. All basic igneous rocks experienced post-magmatic alteration by fluid-rock interaction ranging from processes at the seafloor, in the shallow crust, during subduction zone hydration, in the exhumation channel and late Alpine regional metamorphisms. The consequences of these alteration processes can be identified at various levels in the rock composition data. It was found that the REE data are little affected by fluid-rock alteration. Some trace elements, notably Cs, Rb, and Ba are typically massively altered relative to igneous compositions in all three groups of meta-basalts. Generally, meta-basalts from the TGU and the SMN preserved the features of the original composition whilst the ZSU meta-volcanic rocks experienced massive alteration. For the ZSU meta-volcanic rocks it is evident that Zr was gained and Y lost during high-pressure fluid-rock interaction indicating a mobile behavior of the two elements during HP-metamorphism in contrast to their behavior in hydrothermal near-surface fluid-rock interaction.
    Description: Albert-Ludwigs-Universität Freiburg im Breisgau (1016)
    Keywords: ddc:552.4 ; Meta-basalt ; Meta-gabbro ; Trace elements ; REE patterns ; Ophiolite
    Language: English
    Type: doc-type:article
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  • 10
    Publication Date: 2021-07-26
    Description: Garnet is a prototypical mineral in metamorphic rocks because it commonly preserves chemical and textural features that can be used for untangling its metamorphic development. Large garnet porphyroblasts may show extremely complex internal structures as a result of a polycyclic growth history, deformation, and modification of growth structures by intra- and intercrystalline diffusion. The complex internal structure of garnet porphyroblasts from garnet–phengite schists (GPS) of the Zermatt area (Western Alps) has been successfully decoded. The centimetre-sized garnet porphyroblasts are composed of granulite facies garnet fragments overgrown by a younger generation of grossular-rich eclogite facies garnet. The early granulite facies garnet (G-Grt) formed from low-P, high-T metamorphism during a pre-Alpine orogenic event. The late garnet (E-Grt) is typical of high-pressure, low-temperature (HPLT) metamorphism and can be related to Alpine subduction of the schists. Thus, the garnet of the GPS are polycyclic (polymetamorphic). G-Grt formation occurred at ~670 MPa and 780°C, E-Grt formed at ~1.7 GPa and 530°C. The G-Grt is relatively rich in Prp and poor in Grs, while E-Grt is rich in Grs and poor in Prp. The Alm content (mol.%) of G-Grt is 68 of E-Grt 55. After formation of E-Grt between and around fragmented G-Grt at 530°C, the GPS have been further subducted and reached a maximum temperature of 580°C before exhumation started. Garnet composition profiles indicate that the initially very sharp contacts between the granulite facies fragments of G-Grt and fracture seals of HPLT garnet (E-Grt) have been modified by cation diffusion. The profiles suggest that Ca did not exchange at the scale of 1 µm, whereas Fe and Mg did efficiently diffuse at the derived maximum temperature of 580°C for the GPS at the scale of 7–8 µm. The Grt–Grt diffusion profiles resulted from spending c. 10 Ma at 530–580°C along the P–T–t path. The measured Grt composition profiles are consistent with diffusivities of log DMgFe = −25.8 m2/s from modelled diffusion profiles. Mg loss by diffusion from G-Grt is compensated by Fe gain by diffusion from E-Grt to maintain charge balance. This leads to a distinctive Fe concentration profile typical of uphill diffusion.
    Keywords: 549 ; diffusion ; eclogite facies ; garnet ; porphyroblast ; uphill diffusion
    Language: English
    Type: article
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