Keyphrases
Chilean Andes
100%
El Teniente
100%
Ore Deposits
100%
Hf Isotope Analysis
100%
Hf Isotopes
100%
Magma
100%
Source Evolution
100%
Zircon Trace Elements
100%
Porphyry Cu-Mo
100%
Magmatic Evolution
100%
Zircon
66%
Central Chile
50%
Igneous Rocks
50%
Cenozoic
33%
Crystallization
33%
Cu-Mo
33%
Isotopic Signature
33%
Miocene-Pliocene
33%
Dehydration Melting
33%
Magma Composition
33%
Magmatic Activity
33%
Morphological Characteristics
33%
Subduction-related
33%
Chemical Characteristics
16%
Crustal Contamination
16%
Ti Content
16%
Weighted Mean
16%
Orogen
16%
Cooling Rate
16%
Overgrowth
16%
Andes
16%
In Situ Analysis
16%
Isotopic Characteristics
16%
Inherited Zircon
16%
Margin Setting
16%
Residence Time
16%
Isotopic Composition
16%
Morphological Trends
16%
Magmatism
16%
Compositional Characteristics
16%
Thermal Regime
16%
Convergent Margin
16%
Cathodoluminescence
16%
Y Content
16%
Cenozoic Evolution
16%
Mantle-derived
16%
Arc Migration
16%
Basalt Differentiation
16%
Primary Basalts
16%
Primary Control
16%
Porphyry Copper Mineralization
16%
Whole-rock Composition
16%
U-Pb
16%
Intrusive Rocks
16%
Lower Limit
16%
Range Limits
16%
Element Content
16%
Rare Earth Elements
16%
U-Th
16%
Porphyry Cu Deposit
16%
Porphyry Deposit
16%
Long-lived
16%
Unit Covering
16%
Chemical Trends
16%
High Temperature
16%
Crystallization Temperature
16%
Tectonic Regime
16%
Crustal Thickening
16%
Mantle Zircon
16%
Crustal Thickness
16%
Grain Samples
16%
Juvenile Sources
16%
Earth and Planetary Sciences
Zircon
100%
Andes
100%
Ore Deposit
100%
Trace Element
100%
Magma
100%
Chile
42%
Morphology
42%
Isotopic Composition
42%
Igneous Rock
42%
Miocene
28%
Dehydration Melting
28%
Pliocene
28%
Crustal Contamination
14%
Lithosphere
14%
Basalt
14%
Tectonics
14%
Convergent Margin
14%
Thermal Regime
14%
Crustal Thickening
14%
Magmatism
14%
Homogenizing
14%
Crustal Thickness
14%
Rare Earth Element
14%
Cathodoluminescence
14%