The new study was carried out in the Yerington Batholith of Nevada
A rapid switch in magmatic plumbing taps porphyry copper deposit-forming magmas
Scientists have made a fascinating new discovery about the formation of mineral deposits crucial to our transition to a ‘green economy’.
The new collaborative study, led by Lawrence Carter from the University of Exeter’s Camborne School of Mines, has shown that porphyry-type copper deposits form due to a rapid change in the underlying magmatic plumbing system which forms them.
The study describes a new 4-D model for the formation of porphyry-type copper deposits which challenges the current paradigm of a progressive, multi-million year, arc-scale ramp up in the ‘fertility’, or mineralising potential, of magmatic systems. There may instead be an order of magnitude more rapid switch, over a period of less than 200 kyrs, from the intrusion of non-mineralising to porphyry deposit-forming magmas. The suggested cause of this is a change from magma production in the mid-crust to lower crust, probably initiated by the intrusion of much hotter magmas from the mantle.
The researchers believe that these findings will help exploration geologists discover the next generation of porphyry copper deposits. Porphyry-type deposits provide most of the world’s copper and molybdenum, as well as large amounts of gold and other metals, which are of increasing demand for green technologies such as electric vehicles, wind turbines and solar panels, and for power transmission. As such, they are the principle target of many mining companies worldwide. The problem is that most large near-surface deposits have already been found and therefore geologists are having explore deeper and under thicker layers of younger rocks to find them. There is therefore a growing need to better understand where and how porphyry copper deposits form and for new methods to find them.
The new study was carried out in the Yerington Batholith of Nevada, where tilting of the upper crust has provided one of the world’s best-exposed (~8km deep) sections through a magmatic-hydrothermal system, from the volcanic to plutonic environments, including four porphyry deposits. Because of this, previous studies in the district have underpinned much of the current understanding of how porphyry-type deposits form.
Lawrence Carter, lead author of the study and Associate at Camborne School of Mines, based at the University of Exeter’s Penryn Campus said: “To address the previously fragmented understanding of the magmatic timescales associated with porphyry-deposit formation, we have studied the world’s best exposed porphyry system by integrating field observations and geochemistry with state-of-the-art high precision zircon U-Pb geochronology. We show that magmatic-systems can ‘switch-on’ their ability to form ore deposits due to a rapid change in their magmatic plumbing, tapping a deeper, more volatile-rich, ‘fertile’ zone.”
Lawrence Carter said: “We also show that the distinct ‘fertile’ geochemical signatures associated with ore-forming magmas develop almost instantaneously (<200 kyrs), and are expressed throughout the magmatic system, including in overlying volcanic rocks. This increases our confidence in the resolution of geochemical signatures related to ‘fertile’ systems, immensely enhancing their use as exploration tools for porphyry copper deposits.”
The research was supported by the NERC GW4+ DTP programme, a NERC Isotope Facilities grant, SelFrag AG, the Society of Economic Geologists Foundation and the NERC highlight topic ‘FAMOS’.
The study, entitled ‘A rapid change in magma plumbing taps porphyry copper deposit-forming magmas, is published in the journal Scientific Reports and is available at https://doi.org/10.1038/s41598-022-20158-y
Date: 17 October 2022