Results 41 to 50 of about 1,125 (137)

Geochronological challenges posed by continuously developing tectonometamorphic systems: insights from Rb–Sr mica ages from the Cycladic Blueschist Belt, Syros (Greece). [PDF]

open access: yes, 2016
Is metamorphism and its causative tectonics best viewed as a series of punctuated events or as a continuum? This question is addressed through examination of the timing of exhumation of the Cycladic Blueschist Belt (CBB).
Bond, CE   +3 more
core   +1 more source

Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction [PDF]

open access: yes, 2015
This research was financially co-supported by the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (XDB03010301), the National Key Project for Basic Research of China (2011CB403102 and 2015CB452604), the Chinese National Natural
Cawood, Peter A.   +6 more
core   +1 more source

Developing an inverted Barrovian sequence; insights from monazite petrochronology [PDF]

open access: yesEarth and Planetary Science Letters, 2014
AbstractIn the Himalayan region of Sikkim, the well-developed inverted metamorphic sequence of the Main Central Thrust (MCT) zone is folded, thus exposing several transects through the structure that reached similar metamorphic grades at different times.
Mottram, Catherine M.   +6 more
openaire   +3 more sources

Origin and evolution of the Variscan Léon eclogites: insights from zircon and garnet petrochronology [PDF]

open access: yesEuropean Journal of Mineralogy
Eclogites record the deep burial and exhumation of crustal terranes, which are key tectonic markers in the evolution of orogenic belts. Unraveling the evolution of eclogites and eclogite-bearing terranes may nevertheless be challenging, especially in old
L. Tual   +9 more
doaj   +1 more source

Late Neogene tectonically driven crustal exhumation of the Sikkim Himalaya : Insights from inversion of multithermochronologic data [PDF]

open access: yes, 2016
Apatite fission track and zircon (U-Th)/He data are reported for 34 bedrock samples distributed between the foothills and the topographic crest of the Darjeeling-Sikkim Himalaya.
Coutand, Isabelle   +4 more
core   +1 more source

Paleoproterozoic Reworking of Archean Crust and Extreme Back‐Arc Metamorphism in the Enigmatic Southern Trans‐Hudson Orogen

open access: yesGeophysical Research Letters
The crustal evolution of the southernmost ∼2000–1800 Ma Trans‐Hudson orogen (THO) is enigmatic due to burial by Phanerozoic sediments. We provide new insights through petrochronologic analysis of a paragneiss drill core sample.
Ian W. Hillenbrand   +6 more
doaj   +1 more source

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

Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite

open access: yesGeochemistry, Geophysics, Geosystems, 2020
Deformation in crustal‐scale shear zones occurs over a range of pressure‐temperature‐time (P‐T‐t) conditions, both because they may be vertically extensive structures that simultaneously affect material from the lower crust to the surface, and because ...
T. K. Cawood, J. P. Platt
doaj   +1 more source

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

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

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