Undeformed crystals are shown in blue, whereas increasing internal deformation is highlighted by a progression of green through yellow to red. ( B) GROD angle EBSD map showing that deformation occurs in regions ~2 mm in size that are separated by 1- to 3-mm undeformed areas. The black box indicates the area analyzed by EBSD in (B) to (D). Areas where the mesostasis has been altered are red brown, and they correlate with the location of the deformed regions in (B). The dominant augite phenocrysts impart the green color, whereas mesostasis is black. ( A) Transmitted light image of the MIL 03346 thin section. The nakhlite source location must have two spatially correlated craters, one ~630 Ma old and another, ejecting the meteorites, ~11 Ma ago. Ensuing water-rock interaction focused on shocked mesostasis with a high density of reactive sites. We propose that an impact ~630 Ma ago simultaneously deformed the nakhlite parent rocks and generated liquid water by melting of permafrost. Mesostasis within shocked areas was aqueously altered to phyllosilicates, carbonates, and oxides, suggesting a genetic link between the two processes. Numerical modeling shows that the pattern of deformation is consistent with shock-generated compressive and tensile stresses. Electron backscatter diffraction demonstrates that the meteorites Miller Range 03346 and Lafayette were heterogeneously deformed, leading to localized regions of brecciation, plastic deformation, and mechanical twinning of augite. We test the theory that water-rock interaction was impact driven. Nakhlite meteorites are ~1.4 to 1.3 Ga old igneous rocks, aqueously altered on Mars ~630 Ma ago. 10 Planetary Science Institute, 1700 East Fort Lowell, Suite 106, Tucson, AZ 85719-2395, USA.9 Department of Earth and Planetary Sciences, Western Australia Museum, Locked Bag 49, Welshpool, WA 6986, Australia.
8 Australian Centre for Astrobiology, University of New South Wales, Sydney, NSW 2052, Australia.7 Oxford Instruments Nanoanalysis, High Wycombe HP12 3SE, UK.6 Dipartimento di Scienze della Terra, Università di Pisa, via Santa Maria 53, 56126, Pisa, Italy.5 Department of Earth Sciences, Uppsala University, Uppsala, Sweden.4 School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.3 Australian Centre for Microscopy and Microanalysis, The University of Sydney, NSW 2006, Australia.2 Space Science and Technology Centre, School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, Australia.1 School of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK.The song is also known for the infamous subwoofer video, demonstrating the extremely loud bass.It has a decent dance routine in The Black Eyed Peas Experience.The instrumental, especially the drop part, is the only best part of the song.The music video is well executed and is set in a futuristic setting.The outro in non-radio edit versions is very cheesy and stretches out way too long.Also, the phrase "Gotta get that" was said 16 times.
The word "boom" was said 109 TIMES IN TOTAL!.
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