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Zawartość zarchiwizowana w dniu 2022-12-23

Mass and heat transfer from the Earth's mantle into the crust: helium isotopes, heat flow and tectonics

Cel



The aim of this project is to study mass and heat transfer from the Earth's mantle into the continental crust. This will include sources of melt, duration of thermal anomalies in the crust, the mixing of mantle and crustal fluids and the length and time scales of fluid migration in the crust.

Central to an examination of the problems of mass and heat transfer from the Earth's mantle into the continental crust is the isotope composition of He in terrestrial fluids, as He is a unique tracer of fluids: escape of He from the atmosphere provides negligibly low background of atmospheric contaminant He in fluids; isotopic ratios of 3He/4He in the mantle are some 1000 times higher than those in the continental crust, making mantle contribution easy to identify; He is a chemically inert element and a conservative tracer of. mantle derived melt.

A very large amount of He data, obtained earlier in the NIS, has still not been published. Within the framework of this project, available measurements of He isotope abundances in fluids will be compiled in a global database together with some other physical and chemical properties of the fluids. Some new isotope analysis will also be carried out in key areas. The data base will enable the first World Map (Atlas) of He isotope distribution on the Earth's surface to be produced.

A comparison of this map with the geological and tectonic structure of the continents and heat flow distribution will enable details of crust-mantle interaction processes, which is the basic aim of the project, to be inferred.

The expected results will be an improved understanding of some major geophysical and geochemical anomalies that exist in the Earth's continental crust. There are geophysical anomalies of exceptionally high heat flow and geochemical anomalies of high mantle-derived 3He. The relationship of these anomalies in terms of melt transport and heat transport from the mantle will be further understood.

The results of this research will be communicated through international journals and through a final report including the compiled database.

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Koordynator

University of Cambridge
Wkład UE
Brak danych
Adres
Downing Street
CB2 3EQ Cambridge
Zjednoczone Królestwo

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Koszt całkowity
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