Simon Large
YOU?
Author Swipe
View article: A zircon case for super-wet arc magmas
A zircon case for super-wet arc magmas Open
Arc magmas have higher water contents (2-6 wt.% H 2 O) than magmas generated in other tectonic environments, with a growing body of evidence suggesting that some deep arc magmas may be ‘super-wet’ (>6 wt.% H 2 O). Here, we use thermodynami…
View article: Tectonic and Crustal Processes Drive Multi-Million Year Arc Magma Evolution Leading up to Porphyry Copper Deposit Formation in Central Chile
Tectonic and Crustal Processes Drive Multi-Million Year Arc Magma Evolution Leading up to Porphyry Copper Deposit Formation in Central Chile Open
Subduction zone magmatism is a major control of volcanism, the generation of modern continental crust and the formation of economically important porphyry Cu–(Mo–Au) deposits. Reading the magmatic record of individual arc segments and cons…
View article: Editorial: The fate of volatiles and metals in magmas: volcanic eruptions, plutons and ore deposits
Editorial: The fate of volatiles and metals in magmas: volcanic eruptions, plutons and ore deposits Open
EDITORIAL article Front. Earth Sci., 29 August 2023Sec. Petrology Volume 11 - 2023 | https://doi.org/10.3389/feart.2023.1279960
View article: The Strontian Intrusive Complex: Petrography, Thermobarometry and the Influence of Titanite on Residual Melt Chemistry
The Strontian Intrusive Complex: Petrography, Thermobarometry and the Influence of Titanite on Residual Melt Chemistry Open
Although the evolution of residual melts in magmatic systems controls their eruptability and ore-forming potential, their compositions are obscured in plutonic rocks by a protracted near-solidus evolution and the absence of interstitial gl…
View article: Comment on se-2021-129
Comment on se-2021-129 Open
Middle-Late Jurassic high Sr/Y granitic intrusions are extensively exposed in the Liaodong Peninsula, in the eastern part of the North China Craton (NCC). However, the genesis of the high Sr/Y signature in these intrusions has not been stu…
View article: Resolving changes in arc magma volatile budgets over Myr timescales leading up to porphyry Cu formation 
Resolving changes in arc magma volatile budgets over Myr timescales leading up to porphyry Cu formation  Open
<p>The crustal-scale magmatic systems of Andean-style arcs produce thick volcanic deposits and abundant plutons that are emplaced into the crust. They can also generate spatially- and temporally-restricted, economically-important por…
View article: Petrological and zircon chemical record of arc magma evolution from long-lived batholith construction to giant porphyry copper deposit formation&#160;
Petrological and zircon chemical record of arc magma evolution from long-lived batholith construction to giant porphyry copper deposit formation  Open
<p>Porphyry Cu ore deposits are a rare product of arc magmatism that often form spatiotemporal clusters in magmatic arcs. The petrogenetic evolution of igneous rocks that cover the temporal window prior to and during porphyry Cu depo…
View article: From long-lived batholith construction to giant porphyry copper deposit formation: petrological and zircon chemical evolution of the Quellaveco District, Southern Peru
From long-lived batholith construction to giant porphyry copper deposit formation: petrological and zircon chemical evolution of the Quellaveco District, Southern Peru Open
Porphyry Cu ore deposits are a rare product of arc magmatism that often form spatiotemporal clusters in magmatic arcs. The petrogenetic evolution of igneous rocks that cover the temporal window prior to and during porphyry Cu deposit forma…
View article: Resolving the timescales of magmatic and hydrothermal processes associated with porphyry deposit formation using zircon U–Pb petrochronology
Resolving the timescales of magmatic and hydrothermal processes associated with porphyry deposit formation using zircon U–Pb petrochronology Open
Understanding the formation of economically important porphyry Cu–Au deposits requires knowledge of the magmatic-to-hydrothermal processes that act within the much larger magmatic system and the timescales on which they occur. We apply hig…
View article: Petrochronology resolves the multi-Myr crustal scale magmatic evolution of an arc segment resulting in porphyry copper formation
Petrochronology resolves the multi-Myr crustal scale magmatic evolution of an arc segment resulting in porphyry copper formation Open
<p>The crustal-scale magmatic systems of Andean-style subduction zones produce thick volcanic deposits and abundant plutons emplaced into the upper crust. They can also result in the formation of spatially- and temporally-restricted,…
View article: Resolving the timescales of magmatic and hydrothermal processesassociated with porphyry deposit formation using zircon U-Pb petrochronology
Resolving the timescales of magmatic and hydrothermal processesassociated with porphyry deposit formation using zircon U-Pb petrochronology Open
Understanding the formation of economically important porphyry-Cu-Au deposits requires the knowledge of the magmatic-to-hydrothermal processes that act within the much larger underlying magmatic system and the timescales on which they occu…
View article: Zircon-hosted apatite inclusions: A powerful tool for reconstruction of Cl contents in melts
Zircon-hosted apatite inclusions: A powerful tool for reconstruction of Cl contents in melts Open
Chlorine in the exsolved volatile phase plays an important role in complexing with metals in the extraction and concentration of metals in magmatic-hydrothermal ore deposits. Therefore, tracking the concentration and evolution of Cl in the…
View article: Magma Evolution Leading to Porphyry Au-Cu Mineralization at the Ok Tedi Deposit, Papua New Guinea: Trace Element Geochemistry and High-Precision Geochronology of Igneous Zircon
Magma Evolution Leading to Porphyry Au-Cu Mineralization at the Ok Tedi Deposit, Papua New Guinea: Trace Element Geochemistry and High-Precision Geochronology of Igneous Zircon Open
ISSN:1554-0774
View article: Trace elements in fluid inclusions of sediment-hosted gold deposits indicate a magmatic-hydrothermal origin of the Carlin ore trend
Trace elements in fluid inclusions of sediment-hosted gold deposits indicate a magmatic-hydrothermal origin of the Carlin ore trend Open
The Carlin-type deposits in Nevada (western USA) constitute the world’s second-largest gold ore province. These structurally and stratigraphically controlled, sediment-hosted ore bodies are characterized by carbonate dissolution attending …