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  • 1
    Keywords: Graptolithen ; Tonschiefer
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (IX, 277 Seiten)
    ISBN: 0632010711
    Series Statement: Geological Society special publication 20
    DDC: 563'.71
    Language: Undetermined
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Igneous rocks. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (568 pages)
    Edition: 1st ed.
    ISBN: 9781483289694
    Series Statement: Issn Series ; v.Volume 7
    DDC: 552/.1
    Language: English
    Note: Front Cover -- Igneous Petrology -- Copyright Page -- Table of Contents -- Preface -- Glossary -- CHAPTER 1. MINERALOGY OF IGNEOUS ROCKS -- 1.1. Introduction -- 1.2. Chemical considerations -- 1.3. Factors governing structures of silicate minerals -- 1.4. Principles governing crystalline solution -- 1.5. Nomenclature, composition, and paragenesis of igneous rock-forming minerals -- 1.6. Recognition of minerals in thin section -- CHAPTER 2. VOLCANIC ACTIVITY -- 2.1. Introduction -- 2.2. Volcanic activity described by natural groupings -- 2.3. Fragmental volcanic rocks -- CHAPTER 3. FORMS AND STRUCTURES OF INTRUSIVE ROCKS -- 3.1. Introduction -- 3.2. Basic intrusions into continental crust -- 3.3. Ophiolite association -- 3.4. Subvolcanic and central complexes -- 3.5. Deep-seated granitic rocks -- 3.6. Features to map and sample in intrusive rocks -- CHAPTER 4. CLASSIFICATION OF IGNEOUS ROCKS -- 4.1. Introduction -- 4.2. Presentation of compositional data -- 4.3. Reflection of chemistry in mineralogy -- 4.4. Classification -- CHAPTER 5. PETROGRAPHY OF IGNEOUS ROCKS -- 5.1. Introduction -- 5.2. Procedure -- 5.3. A working vocabulary -- CHAPTER 6. PHYSICAL PROPERTIES AND PHYSICAL CHEMISTRY OF MAGMAS -- 6.1. Physical properties of magma -- 6.2. Kinetics of crystallization of magma -- 6.3. Studies in the equilibrium crystallization of synthetic melts and their bearing on magmatic cooling history, igneous rock compositions and textures -- CHAPTER 7. DIFFERENTIATION OF IGNEOUS ROCKS -- 7.1. Introduction -- 7.2. Differentiation processes within liquid magma -- 7.3. Hybridization -- 7.4. Assimilation -- 7.5. Autometasomatism -- 7.6. Crystal fractionation -- CHAPTER 8. IGNEOUS ROCK SERIES -- 8.1. Historical review -- 8.2. Definition of terms -- 8.3. Tholeiite and alkali basalt -- 8.4. Thermodynamic basis of classification based on silica activity. , 8.5. Basis of classification of igneous rock series followed in this book -- 8.6. Useful parameters, indices and variation diagrams -- 8.7. Complications affecting simple fractionation models -- CHAPTER 9. IGNEOUS ROCKS OF OCEANIC AREAS -- 9.1. Oceanic crust -- 9.2. Mid-ocean ridge basalts (MORB) -- 9.3. Oceanic island tholeiites (OIT) -- 9.4. Alkali basalt series and basanites -- 9.5. Highly alkaline rocks of oceanic islands -- CHAPTER 10. IGNEOUS ROCKS OF CONTINENTAL AREAS -- 10.1. Introduction -- 10.2. Kimberlites and related rocks -- 10.3. Carbonatites -- 10.4. Highly potassium-rich series -- 10.5. Various alkaline series as exemplified by igneous activity in the Kenya dome . -- 10.6. Igneous activity in the Afro-Arabian dome associated with plate separation . . -- 10.7. Continental flood basalts mainly of tholeiitic composition -- 10.8. Intrusive rocks of anorogenic continental terrain -- 10.9. Conclusions -- CHAPTER 11. IGNEOUS ROCKS ABOVE BENIOFF SEISMIC ZONES -- 11.1. Introduction -- 11.2. Variation among young SBZ volcanic rocks -- 11.3. Plutonic rocks apparently formed during SBZ eruptive activity -- CHAPTER 12. IGNEOUS ROCKS OF THE PRECAMBRIAN . . -- 12.1. Introduction -- 12.2. Extraterrestrial igneous rocks -- 12.3. Astroblemes and related igneous activity on the Earth -- 12.4. Archaean igneous rocks -- 12.5. Igneous activity in Proterozoic time -- CHAPTER 13. PETROGENESIS OF IGNEOUS ROCKS -- 13.1. Introduction -- 13.2. Composition of upper mantle -- 13.3. Experimental work -- 13.4. The mantle-magma system -- 13.5. Trace elements in mafic rocks -- 13.6. Status of parental magma in petrogenetic work -- 13.7. Conclusions -- CHAPTER 14. DEGRADATION OF IGNEOUS ROCKS -- 14.1. Introduction -- 14.2. Spilite and keratophyre -- 14.3. Metasomatism in degraded volcanic rocks -- 14.4. Determination of magmatic affinity of degraded volcanic rocks. , 14.5. Discussion -- EPILOGUE -- REFERENCES -- NAME INDEX -- LOCALITY INDEX -- GENERAL INDEX.
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  • 3
    Book
    Book
    London [u.a.] : Chapman & Hall
    Keywords: Geology and Palaeontology ; Soil mechanics Congresses ; Clay Congresses ; Geochemistry Congresses ; Fluid dynamics Congresses ; Kongreß Konferenz ; soil mechanics ; clay ; geochemistry ; fluid dynamics ; Konferenzschrift ; Tonmineralogie ; Geochemie ; Tonmineral ; Porosität ; Abdichtung ; Barriere ; Speichergestein ; Ton ; Strömungsmechanik ; Ton
    Type of Medium: Book
    Pages: XV, 427 S. , graph.Darst.
    Edition: 1.ed.
    ISBN: 0412489805
    Series Statement: The Mineralogical Society series 4
    DDC: 551.9
    RVK:
    Language: English
    Note: Literaturangaben
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  • 4
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    In:  EPIC3In: Ocean Circulation and Climate / G. Siedler, J. Church and J. Gould, eds. New York : Academic Press. p., pp. 271-302, ISBN: 0-12-641351-7
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
    Format: application/pdf
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  • 5
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    In:  EPIC3Berichte aus dem Fachbereich Physik No. 94, Alfred-Wegener-Institut, Bremerhaven
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev
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  • 6
    Publication Date: 2019-07-16
    Description: The GRACE satellite mission observes the gravity field of the Earth with unprecedented accuracy. Gravity field products provided by the GRACE Science Data System allow to assess both the static geoid, as well as time-varying signals associated with changes of global water mass distribution. For estimating the capability of spaceborne gravity measurements to detect the temporal variability of oceanic mass distribution and currents, the GRACE data is validated against in-situ measurements of ocean bottom pressure (OBP) provided by Pressure Sensors located at the sea floor.In the framework of a joint BMBF (German Ministry for Education and Research) project, a database that includes globally available OBP observations is presented here. This database is used to carry out a comprehensive ground-truth validation of GRACE. The capability of GRACE solutions from different analysis centers to capture oceanic mass variability is assessed by comparisons with in-situ OBP data from the Southern Ocean, Atlantic, Indian and Pacific Oceans. It is shown, that GRACE detects real oceanic variability in regions with a high signal-to-noise ratio (e.g. the Antarctic Circumpolar Current), and that reduced noise levels of more recent GRACEsolutions may improve GRACE performance in other parts of the Ocean (e.g. the tropical Atlantic). The ground-truth validation against OBP aids the further improvement of GRACE data processing that in the future GRACE may be used to monitor geostrophic transport variability and water mass changes on a global scale.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
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    ESA
    In:  EPIC3Proceedings of OceanObs09: Sustained Ocean Observations and Information for Society (Vol. 2), Venice, Italy, 21-25 September 2009, Hall, J., Harrison D.E. & Stammer, D., Eds., ESA Publication WPP-306., Proceedings of OceanObs’09: Sustained Ocean Observations and Information for Society (Vol. 2), ESA, Public
    Publication Date: 2017-07-04
    Description: The tools of geodesy have the potential to transform the Ocean Observing System. Geodetic observations are unique in the way that these methods produce accurate, quantitative, and integrated observations of gravity, ocean circulation, sea surface height, ocean bottom pressure, and mass exchanges among the ocean, cryosphere, and land. These observations have made fundamental contributions to the monitoring and understanding of physical ocean processes. In particular, geodesy is the fundamental science to enable determination of an accurate geoid model, allowing estimate of absolute surface geostrophic currents, which are necessary to quantify ocean’s heat transport. The present geodetic satellites can measure sea level, its mass component and their changes, both of which are vital for understanding global climate change. Continuation of current satellite missions and the development of new geodetic technologies can be expected to further support accurate monitoring of the ocean. The Global Geodetic Observing System (GGOS) of the International Association of Geodesy (IAG) provides the means for integrating the geodetic techniques that monitor the Earth's time-variable surface geometry (including ocean, hydrologic, land, and ice surfaces), gravity field, and Earth rotation/orientation into a consistent system for measuring ocean surface topography, ocean currents, ocean mass and volume changes. This system depends on both globally coordinated ground-based networks of tracking stations as well as an uninterrupted series of satellite missions. GGOS works with the Group on Earth Observations (GEO), the Committee on Earth Observation Satellites (CEOS) and space agencies to ensure the availability of the necessary expertise and infrastructure. In this white paper, we summarize the community consensus of critical oceanographic observables currently enabled by geodetic systems, and the requirements to continue such measurements. Achieving this potential will depend on merging the remote sensing techniques with in situ measurements of key variables as an integral part of the Ocean Observing System.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Book , peerRev
    Format: application/pdf
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  • 8
    Publication Date: 2019-04-26
    Description: The west Antarctic Peninsula (WAP) region has undergone significant changes in temperature and seasonal ice dynamics since the mid-twentieth century, with strong impacts on the regional ecosystem, ocean chemistry and hydrographic properties. Changes to these long-term trends of warming and sea ice decline have been observed in the 21st century, but their consequences for ocean physics, chemistry and the ecology of the high-productivity shelf ecosystem are yet to be fully established. The WAP shelf is important for regional krill stocks and higher trophic levels, whilst the degree of variability and change in the physical environment and documented biological and biogeochemical responses make this a model system for how climate and sea ice changes might restructure high-latitude ecosystems. Although this region is arguably the best-measured and best-understood shelf region around Antarctica, significant gaps remain in spatial and temporal data capable of resolving the atmosphere-ice-ocean-ecosystem feedbacks that control the dynamics and evolution of this complex polar system. Here we summarise the current state of knowledge regarding the key mechanisms and interactions regulating the physical, biogeochemical and biological processes at work, the ways in which the shelf environment is changing, and the ecosystem response to the changes underway. We outline the overarching cross-disciplinary priorities for future research, as well as the most important discipline-specific objectives. Underpinning these priorities and objectives is the need to better-define the causes, magnitude and timescales of variability and change at all levels of the system. A combination of traditional and innovative approaches will be critical to addressing these priorities and developing a co-ordinated observing system for the WAP shelf, which is required to detect and elucidate change into the future.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 9
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Langmuir 7 (1991), S. 2419-2421 
    ISSN: 1520-5827
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1432-1041
    Keywords: Congestive heart failure ; Captopril ; sublingual ; pharmacokinetic ; pharmacodynamic
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Abstract Objective: The pharmacokinetics and pharmacodynamics of buffered sublingual captopril were assessed in patients with congestive heart failure (CHF). Methods: The study was carried out in a randomised single-blind cross-over fashion (n=6, 4 males and 2 females) and involved two study days, at least 7 days apart. Baseline measurements were carried out for plasma renin activity (PRA), blood pressure (B.P.) and heart rate (H.R.). Captopril (12.5 mg) was administered sublingually with dibasic potassium phosphate which maintained salivary pH at 7, or perorally with 100 ml of water. Further B.P., H.R. measurements and venous blood samples were taken over a 3 hour period post-drug administration. Blood samples were analysed for captopril and PRA levels. Results: tmax after buffered sublingual administration of captopril, which ranged from 40–60 min (median=40 min), was significantly shorter than after peroral administration (range 60–120 min, median=90 min). Cmax was slightly greater after buffered sublingual than after peroral administration with mean values of 108.2 vs. 94.0 ng·ml−1. AUC values were similar after both routes of administration. Systolic and diastolic B.P. vs. time profiles for each administration method were significantly different i.e. sublingual administration produced an earlier reduction in B.P., however, HR did not differ significantly between the two routes. Conclusion: The data indicate that this novel administration method of captopril leads to an increased rate, but an unchanged extent of captopril absorption, suggesting a modest therapeutic advantage with the use of buffered sublingual captopril if a rapid reduction in blood pressure is required.
    Type of Medium: Electronic Resource
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