- Clay minerals in late glacial and Holocene sediments of the northern and southern Aegean Sea
- Crustal contamination of mafic magmas: evidence from a petrological, geochemical and SrNdOsO isotopic study of the
- A geochemical and Sr-Nd-O isotopic study of the Proterozoic Eriksfjord Basalts, Gardar Province, South
- Principal agent of energy and mass exchange between the ocean and the Earth's crust
- Geochemical and isotopic constraints on the petrogenesis of granitoids from the Dalat zone, southern Vietnam
- N. Jb. Miner. Abh. Fast Track DOI: 10.1127/0077-7757/2006/0058 Fast Track Article by E. Schweizerbart'sche Verlagsbuchhandlung 2006
- Sm-Nd method 147Sm decays to 143Nd by -decay,
- Ar-ages of phlogopite in mantle xenoliths from South African kimberlites: Evidence for metasomatic mantle impregnation during the Kibaran orogenic cycle
- Geochemie der Kruste Element distribution between crust and mantle
- U-Th-Pb Method Method is based on the following three decay reactions
- 6. Sedimentation rates Frank et al. 2008
- Einfhrung in die Geochemie Radiometrische Datierung
- PUBLISHED ONLINE: 22 NOVEMBER 2009 | DOI: 10.1038/NGEO695 Prolonged mantle residence of zircon xenocrysts
- ORIGINAL PAPER From emplacement to unroofing: thermal history
- Mineralogy and Petrology (2006) 86: 4562 DOI 10.1007/s00710-005-0091-7
- ORIGINAL PAPER Wolfgang Siebel Ulrich Blaha Fukun Chen
- PillowPillow--lavalava Columbia River Basalt
- ORIGINAL PAPER Age constraints on faulting and fault
- ORIGINAL PAPER Zircon Hf isotope perspective on the origin of granitic rocks
- Tectono-metamorphic evolution of the Wadi Hafafit Culmination (central Eastern Desert, Egypt). Implication for Neoproterozoic
- Geomaterials Archean inheritances in the pyroxeneamphibole-bearing gneiss
- Two Distinctive Granite Suites in the SW Bohemian Massif and their Record of
- Tectonic implications of new UPb zircon ages of the Ladakh batholith, Indus suture zone, northwest Himalaya, India
- Chemie der Erde 67 (2007) 151174 Petrology, geochemistry and zircon age for redwitzite at Abertamy,
- Geochemical Journal, Vol. 41, pp. 29 to 45, 2007 *Corresponding author (e-mail: fukun-chen@mail.igcas.ac.cn)
- The magmatic evolution of the Land's End pluton, Cornwall, and associated pre-enrichment of metals
- The Grnnedal-Ika CarbonatiteSyenite Complex, South Greenland: Carbonatite
- Chemie der Erde 65 (2005) 4778 Geochemical and isotopic characteristics and evolution of the
- Sr isotope systematics of K-feldspars in plutonic rocks revealed by the RbSr microdrilling technique
- ORIGINAL PAPER Gu ltekin Topuz Rainer Altherr
- TTG magmatism in the Congo craton; a view from major and trace element geochemistry, RbSr and SmNd systematics: case
- Zircon Pb-Pb and U-Pb systematics of TTG rocks in the Congo Craton: Constraints on crust formation, magmatism, and Pan-African lead loss
- Provenance of the Beihuaiyang lower-grade metamorphic zone of the Dabie ultrahigh-pressure collisional orogen, China: evidence
- Int J Earth Sci (Geol Rundsch) (2003) 92:3653 DOI 10.1007/s00531-002-0305-8
- Isotope systematics of ore-bearing granites and host rocks of the Orlovka-Spokoinoe mining
- partial melting yields magmas of different composition than melting rock at zones of upwelling (oceanic ridges) ultramafic rock (peridotite) partially melts
- Growth and differentiation of the Earth`s continental crust
- Granitoids and continental crust
- Analytical methods in radiogenic isotope
- The Rb-Sr method Based on the decay reaction
- Lu-Hf method 176Lu decays to 176Hf by -decay,
- U-Th-Pb method Method is based on the following three decay reactions
- Terrestrial cosmogenic isotopes Great impact on environmental and earth sciences over the
- Applications 1/2 1. Dating Quaternary basalt volcanism
- How we know what's inside the Earth ? Astronomy -Physics
- 3. Geowissenschaftlich wichtige Elemente Erdalkalimetalle, Leichte Elemente
- Parent--daughter system: D Number of daughter atoms, today
- 24. May 2011 Wolfgang Siebel
- Plate TectonicsPlate Tectonics Plate TectonicsPlate Tectonics
- Hydrothermal activity Hydrothermal circulation at mid-ocean ridges
- The major element chemistry of MORBs
- Trace ElementsTrace Elements REE diagram for MORBs
- N-MORBs: 87Sr/86Sr < 0.7035 and 143Nd/144Nd > 0.5130, depleted mantle source
- Primordial noble gases: 3He, 20Ne, 36Ar, 130Xe Produced by radioelement decay: 4He, 21Ne,
- Ozean als Reservoir Chemische Zusammensetzung von Meerwasser weicht stark von der
- Fr skulares Gleichgewicht gilt: bzw. Ai = iNi
- Int J Earth Sci (Geol Rundsch) (2004) 93:329340 DOI 10.1007/s00531-004-0387-6
- Late Proterozoic magmatism and metamorphism recorded in gneisses from the Dabie high-pressure metamorphic zone,
- Open system model of Pb isotope evolution of Galer & O'Nions (1985) Nature 316Galer & O'Nions (1985) Nature 316
- Ocean crust reaching a subduction zone is
- Subduction zones Melt formation and crustal growth
- ORIGINAL PAPER Archaean high-K granitoids produced by remelting of earlier
- G. Faure: Principles of Isotope Geology (3. Aufl. 2005) A. Dickin: Radiogenic Isotope Geology (2005)
- "U-Pb" method Boltwood studied "radioactive series," and found
- Grter Naturraum der Erde (71 % der Erdoberflche) Wichtigstes Reservoir des globalen Wasserkreislaufs (94 % allen Wassers)
- Age and emplacement of late-Variscan granites of the western Bohemian Massif with main focus on the Hauzenberg granitoids
- Lecture scheduleLecture schedule Introduction; Marine geology
- QzAlkalibasalte Alkalibasalte: Nephelin -Diopsid -Forsterit -Albit
- OIBs evolution in the series Tholeiitic, alkaline, and highly alkaline
- Al ist das hufigste Metall der Erdkruste Al ist nahezu unlslich whrend der Verwitterung
- doi:10.1016/j.gca.2003.12.008 Nd-, O-, and H-isotopic evidence for complex, closed-system fluid evolution of the
- Earth and Moon Neighbors http://www.geokem.com/lunar.html
- Diffusion in minerals and melts Surface diffusion essentially over a 2 dimensional
- Zircon ages and NdHf isotopic composition of the Zhaertai Group (Inner Mongolia): Evidence for early Proterozoic evolution
- Be is a particle reactive element becomes
- Petrogenesis of the Linxi granitoids, northern Inner Mongolia of China: Constraints on basaltic underplating
- Ozeanographie, Meereskunde Physikalische Ozeanographie (ozeanographische Messverfahren)
- [The Journal of Geology, 2007, volume 115, p. 215230] 2007 by The University of Chicago. All rights reserved. 0022-1376/2007/11502-0008$15.00 Geochronological and Petrological Constraints for Tectonic
- bersicht Teil II: 1. Grundlagen
- N. Jb. Miner. Abh. Fast Track DOI: 10.1127/0077-7757/2006/0057 Fast Track Article by E. Schweizerbart'sche Verlagsbuchhandlung 2006
- Isotope GeochemistryIsotope Geochemistry Isotopes do not fractionate during partial
- Geochemical classification of elements Chemie fr Geowissenschaftler
- Das Finnigan MAT 262 Massenspektrometer in der Geochemie
- Innertropische Konvergernz quatorialstrme
- The Earth's Interior How we know what's inside?
- Spallation reactions: 16O(n,4p3n)10Be
- How does the mantle melt?How does the mantle melt? 1) Increase the temperature
- How many years must a mountain exist Before it is washed to the Sea?
- Geochemical Journal, Vol. 40, pp. 149 to 159, 2006 *Corresponding author (e-mail: fukun-chen@mail.igcas.ac.cn)
- ORIGINAL PAPER Zircon age and NdHf isotopic composition of the Yunnan
- Two Distinctive Granite Suites in the Southwestern Bohemian Massif: Reply to
