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Multi-Method (Geo-) Thermochronology and Trace Elements Tracing Magmatism, Mineralization and Tectonic Evolution

With the rapid development of analytical techniques, especially the in situ Lu-Hf, Rb-Sr, U-Pb, fission-track, and (U-Th)/He dating of garnet, zircon, apatite, and other accessory minerals, several important geological issues have been successfully resolved or re-determined in the past decade. Among...

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Format: Online
Sprog:engelsk
Udgivet: MDPI - Multidisciplinary Digital Publishing Institute 2025
Fag:
A1-type granite
high oxygen fugacity
adakitic rocks
Laoshan suite
Jiaodong Peninsula
Daliuhang gold deposit
in situ sulfur isotopes
H–O–Pb–He–Ar isotopes
pyrite Rb–Sr isochron age
zircon U–Pb age
Xuebaoding
scheelite
mineralogy characteristics
in situ elements analysis
Sr-Nd isotopes
pyrite
spectroscopic characteristics
geochemical characteristics
?34S stable isotopes
Fukang Sag
geothermal gradient
heat flow
thermochronometry
thermal history
tectono-thermal evolution
maturity evolution
crude oil
gold
affinity
organic acid
gold deposit
offshore of Northern Sanshandao
in-situ sulfur isotopes
pyrite trace elements
Rb–Sr isochron age
geochemical anomaly recognition
Shapley values
interpretability technique
gold deposits
west Qinling
Sinai tectonic history
the Arabian–Nubian shield
rift flanks
Egypt thermochronology
LA-ICP-MS
Indo-Burma Range
Myanmar
Argoland
Neotethys Ocean
microcontinent
Triassic
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
Online adgang:ONIX_20250812T095121_9783725834068_194
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Summary:With the rapid development of analytical techniques, especially the in situ Lu-Hf, Rb-Sr, U-Pb, fission-track, and (U-Th)/He dating of garnet, zircon, apatite, and other accessory minerals, several important geological issues have been successfully resolved or re-determined in the past decade. Among these, the precise temporal evolution and duration of magmatism and mineralized processes, as well as the uplift and exhumation history of mineral deposits and basins within orogenic belts and cratons, can assist the exploration of mineral and petroleum resources. Moreover, in situ mineral-scale trace element concentrations could also be simultaneously determined using LA-ICP-MS in situ accessory mineral dating. This would provide new perspectives on the formation and evolution of major geological objects via integration with corresponding ages. Although previous studies have focused on most scientific issues of magmatism, mineralization, and tectonic evolution in different geological objects, several aspects of these investigations have not previously shown agreement. This Special Issue collects contributions related to the field of petrology, mineralogy, and mineral deposits as well as sedimentology and tectonics based on state-of-the-art analytical techniques. This reprint will contribute to a better understanding of scientific issues of magmatism, mineralization, and tectonic evolution in different geological objects.

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