Results 61 to 70 of about 1,181 (167)

Thermokinematic evolution of the Annapurna-Dhaulagiri Himalaya, central Nepal: The composite orogenic system [PDF]

open access: yes, 2016
The Himalayan orogen represents a ‘‘Composite Orogenic System’’ in which channel flow, wedge extrusion, and thrust stacking operate in separate ‘‘Orogenic Domains’’ with distinct rheologies and crustal positions.
Baëta R. D.   +14 more
core   +2 more sources

Interpreting Europium Anomalies in Zircon: The Importance of Source Redox

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 10, October 2025.
Abstract The sources of granitoids are variably oxidized due to the diversity of environments in which they form. This environmental and consequent chemical variability leads to differences in mineral assemblages, proportions, and compositions of ferric and ferrous iron‐bearing phases in these sources and in the resultant granitoids. Accessory minerals
Chris Yakymchuk, Christopher L. Kirkland
wiley   +1 more source

Tracking Cu‐Fertile Sediment Sources via Multivariate Petrochronological Mixture Modeling of Detrital Zircons

open access: yesJournal of Geophysical Research: Earth Surface, Volume 130, Issue 10, October 2025.
Abstract Whereas the ability to acquire petrochronological data from detrital minerals has exploded, development of tools to analyze and interpret the multivariate data sets has not kept pace. Herein, we present a case study, which applies the recently developed non‐negative Tucker‐1 decomposition (NNT1) method to a multivariate detrital zircon data ...
Joel E. Saylor   +4 more
wiley   +1 more source

Recent advances in petrochronology: from dates to ages and rates of deep orogenic processes

open access: yesComptes Rendus. Géoscience
In order to decipher the prevalent processes active at depth in orogenic systems, their time sequence and their rates have to be assessed. This is essentially done via absolute dating of accessory and rock-forming metamorphic minerals. The interpretation
Labrousse, Loic   +4 more
doaj   +1 more source

Tectonics and crustal evolution [PDF]

open access: yes, 2016
We thank the Natural Environment Research Council (grants NE/J021822/1 and NE/K008862/1) for funding.The continental crust is the archive of Earth's history.
Cawood, Peter A.   +2 more
core   +4 more sources

Seeing through the Ottawan Overprint, Adirondack Mtns., NY: Integrating Microstructural Analysis, Geothermobarometry, and in-situ Monazite Petrochronology [PDF]

open access: yes, 2020
Integrating field observation with petrochronology is critical for understanding the tectonometamorphic evolution of the North American Grenville Province.
Mistikawy, Justin
core   +3 more sources

Petrochronology and Statistical Analysis to Integrate Different Types of Data to Solve Complex Earth Systems Problems [PDF]

open access: yes, 2022
Complex Earth systems problems, like reconstructing orogens and calibrating the geologic time scale, require investigations that link time to geologic processes.
Harrigan, Claire Ostwald
core   +1 more source

Contextualising the Permian Sumdo eclogite belt, Lhasa block, Tibet [PDF]

open access: yes, 2013
HKT-ISTP 2013 ...
Chung, S.   +5 more
core  

Tectonic Setting and Evolution of Anatectic Melt Composition During Prograde Metamorphism up to UHT Metamorphism: Constraints From P–T–t–Melting Path From Rundvågshetta, Lützow–Holm Complex, East Antarctica

open access: yesJournal of Metamorphic Geology, Volume 43, Issue 5, Page 467-495, June 2025.
ABSTRACT The pressure–temperature–time (P–T–t) evolution of a metapelitic ultrahigh‐temperature (UHT) granulite from Rundvågshetta (Lützow–Holm Complex, East Antarctica) and chemical evolution of partial melt during the prograde metamorphism up to UHT metamorphism are studied in detail.
Kota Suzuki   +6 more
wiley   +1 more source

Rift‐Related Low‐Pressure–High‐Temperature Granulite Facies Metamorphism Generates Widespread Peraluminous Crustal Melts: Evidence From the Early Jurassic Mexican Crust

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 5, May 2025.
Abstract High heat fluxes occurring in rift settings are expected to generate partially melted low‐pressure–high‐temperature granulites (LP–HTG). Therefore, studying these rocks can offer valuable insights into crustal reworking during extension. However, our interpretations are limited by the rarity of LP–HTG in the metamorphic record.
Anthony Ramírez‐Salazar   +4 more
wiley   +1 more source

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