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Zircon dating of oceanic crustal accretion

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It emphasizes fundamentals and systematics, historical perspective, analytical methods, data interpretation, and some applications chosen from the literature. Experimental data for zircon saturation show that granodioritic to granitic melts reach zircon saturation at temperatures well above the solidus and therefore could carry significant amounts of early-crystallized zircon during remobilization and transport of magma Watson and Harrison, ; Boehnke et al. However, an increasing number of studies from both plutonic and volcanic rocks reveal complexities in zircon age populations that are difficult to interpret in terms of emplacement time e. This book complements existing coverage by expanding on those parts of isotope geochemistry that are concerned with dates and rates and insights into Earth and planetary science that come from temporal perspectives. Geochronology and Thermochronology offers chapters covering: In essence, the ability of zircon to retain age information at magmatic temperatures — which itself makes zircon such an attractive geochrometer in magmatic systems — also increases its propensity to record protracted crystallization and recycling that obscure the connection between zircon date and magma emplacement rates. One approach to this problem is to target zircon populations included within specific phases versus the bulk rock, and combine those data with petrologic observations and zircon saturation and phase equilibria modeling to estimate the solidification age of certain pulses see Barboni and Schoene, , for an example using the SA. It provides modern perspectives on the current state-of-the art in most of the principal areas of geochronology and thermochronology, while recognizing that they are changing at a fast pace. As a consequence, the physical integrity and also age information in zircon can survive transport, reheating, and reincorporation in subsequent batches of magma, and interpreting zircon dates in terms of magmatic processes is difficult Lissenberg et al. Offers a foundation for understanding each of the methods and for illuminating directions that will be important in the near future Presents the fundamentals, perspectives, and opportunities in modern geochronology in a way that inspires further innovation, creative technique development, and applications Provides references to rapidly evolving topics that will enable readers to pursue future developments Geochronology and Thermochronology is designed for graduate and upper-level undergraduate students with a solid background in mathematics, geochemistry, and geology. Read an interview with the editors to find out more:

Zircon dating of oceanic crustal accretion


In essence, the ability of zircon to retain age information at magmatic temperatures — which itself makes zircon such an attractive geochrometer in magmatic systems — also increases its propensity to record protracted crystallization and recycling that obscure the connection between zircon date and magma emplacement rates. Experimental data for zircon saturation show that granodioritic to granitic melts reach zircon saturation at temperatures well above the solidus and therefore could carry significant amounts of early-crystallized zircon during remobilization and transport of magma Watson and Harrison, ; Boehnke et al. One approach to this problem is to target zircon populations included within specific phases versus the bulk rock, and combine those data with petrologic observations and zircon saturation and phase equilibria modeling to estimate the solidification age of certain pulses see Barboni and Schoene, , for an example using the SA. It emphasizes fundamentals and systematics, historical perspective, analytical methods, data interpretation, and some applications chosen from the literature. Read an interview with the editors to find out more: This book complements existing coverage by expanding on those parts of isotope geochemistry that are concerned with dates and rates and insights into Earth and planetary science that come from temporal perspectives. It provides modern perspectives on the current state-of-the art in most of the principal areas of geochronology and thermochronology, while recognizing that they are changing at a fast pace. As a consequence, the physical integrity and also age information in zircon can survive transport, reheating, and reincorporation in subsequent batches of magma, and interpreting zircon dates in terms of magmatic processes is difficult Lissenberg et al. However, an increasing number of studies from both plutonic and volcanic rocks reveal complexities in zircon age populations that are difficult to interpret in terms of emplacement time e. Offers a foundation for understanding each of the methods and for illuminating directions that will be important in the near future Presents the fundamentals, perspectives, and opportunities in modern geochronology in a way that inspires further innovation, creative technique development, and applications Provides references to rapidly evolving topics that will enable readers to pursue future developments Geochronology and Thermochronology is designed for graduate and upper-level undergraduate students with a solid background in mathematics, geochemistry, and geology. Geochronology and Thermochronology offers chapters covering:

Zircon dating of oceanic crustal accretion


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