Topographic data are draped over infrared image data showing complex tectonic structures and volcanic deposits in the Eridania region of Mars. Warm colours are higher elevation. Image Credit: NASA/Mars Odyssey/HRSC.

Traditionally, Mars has been known to have large shield volcanoes similar to those in Hawaii. However, it was not known that Mars also possessed the diverse, explosive volcanoes that form on Earth due to crustal recycling.

The recent research conducted by Professor Michalski and his international team discover a vast number of diverse volcanoes in the ancient crust of Mars. 'We have known for decades that Mars has volcanoes, but most of the recognised volcanoes correspond to large basaltic shield volcanoes similar to the ones that make up Hawaii,' he explains. 'In this work, we show that the ancient crust has many other types of volcanoes such as lava domes, stratovolcanoes, calderas and large shields of ash, not lava. Further, most scientists see Mars as a planet composed of basalt, which has low silica content and represents little crustal evolution, but these volcanoes have high silica content which means they formed from a complex process of magma evolution not known before.'

The paper suggests that intense volcanism occurred on ancient Mars, causing the crust to collapse into the mantle, where the rocks re-melted, resulting in magmas that have high silica. This tectonic process, called vertical tectonics, is hypothesised to have occurred on the ancient Earth, but rocks on Earth from that period (the Archean, more than 3 billion years ago) are highly modified by later geological activity, so we cannot see evidence for this process clearly on this planet. Therefore, exploring other planets like Mars, which has volcanism but no plate tectonics, can help reveal the mysteries of early crustal recycling on both the Red Planet, and by analogy, on early Earth.

Professor Michalski concluded, 'Mars contains critical geological puzzle pieces that help us understand not only that planet, but the Earth as well. Martian volcanism is much more complex and diverse than has been previously thought.'

'This is a significant discovery because it has revealed that crustal recycling can occur not only in plate tectonic regimes dominated by horizontal movements, but can also occur in pre-plate tectonic regimes dominated by vertical movements. This finding can help earth scientists revolve the long-term controversial issues of how and when felsic continents formed in our planet (Earth)', said Professor Guochun ZHAO, the Chair Professor of HKU Earth Sciences.

The journal paper can be accessed here: https://www.nature.com/articles/s41550-023-02191-7^[2]

About Professor Joseph Michalski A Professor in the Department of Earth Sciences and Deputy Director of the Laboratory for Space Research at HKU, he collaborated with colleagues from mainland China and USA on this research project. He is a Research Fellow of the Hong Kong Research Grants Council, and winner of a Tencent Xplorer Prize in 2023. The funding for this work was provided by the RGC Collaborative Research Fund.

For more information on Professor Joseph Michalski's research, please visit: http://www.clays.space^[3]; Twitter: @JoePlanets

Image and caption for download: https://www.scifac.hku.hk/press^[4]

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References

1. ^{^} Media OutReach Newswire (www.media-outreach.com)
2. ^{^} https://www.nature.com/articles/s41550-023-02191-7 (www.nature.com)
3. ^{^} http://www.clays.space (www.clays.space)
4. ^{^} https://www.scifac.hku.hk/press (www.scifac.hku.hk)