igneous rock Archives

Characterization of a section from the fracture surface to the rock interior. A Photo of the section with a yellow arrow pointing to the fracture surface. B Microscopic image of a region of the section highlighted in a yellow rectangle in A. C Fluorescence microscopy image of the region highlighted by orange rectangle in B. Intensity maps of the section at 1000 cm−1 (D), 1530 cm−1 (E), and 1640 cm−1 (F) obtained by optical photothermal infrared (O-PTIR) spectroscopy. The intensity maps were obtained from the area highlighted with a yellow square in B. G RGB color synthesis of the three intensity maps. A yellow rectangle in G indicates an area where the intensity maps for RGB color synthesis are obtained in Fig. 5A -- Springer Nature

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Subsurface Microbial Colonization at Mineral-Filled Veins in 2-Billion-Year-Old Mafic Rock from the Bushveld Igneous Complex, South Africa

by Keith CowingOctober 27, 2024October 27, 2024

Recent advances in subsurface microbiology have demonstrated the habitability of multi-million-year-old igneous rocks, despite the scarce energy supply from rock-water interactions.

igneous rock

Subsurface Microbial Colonization at Mineral-Filled Veins in 2-Billion-Year-Old Mafic Rock from the Bushveld Igneous Complex, South Africa

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SwRI Study Found Primordial Mini-moons May Explain Meteorite Composition

The Galactic Centre G+0.633-0.0604 Molecular Cloud: A New Astrochemical Gold Mine. I. Gas Physical Properties

Researchers Confirm The Cause Of Earth’s Biggest Mass Extinction