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Ultramafic Rocks from the Mid-Atlantic Ridge
Nature, 1968ACCORDING to the ideas of Hess1 the backbone of active mid-oceanic ridges should consist of peridotites which originated in the Earth's mantle and were subsequently upthrusted into the crust along the axis of ridges, above the up welling limbs of mantle's thermal convection cells.
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Aqueously altered igneous rocks sampled on the floor of Jezero crater, Mars
Science, 2022Ken Farley +2 more
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Radionuclide transport in multi-scale fractured rocks: A review
Journal of Hazardous Materials, 2022Xiaoying Zhang +2 more
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Faulting Processes Unveiled by Magnetic Properties of Fault Rocks
Reviews of Geophysics, 2020Tao Yang, Yu-Min Chou, Eric C Ferré
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