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Mineral Crystallisation in Chondrules (An - SiO2 - Fo including binary systems)
⏲ 5 min 89 sec ✓ 08-May-2019
HiClip: The Color Palette of Nilosyrtis Mensae
⏲ 45 sec ✓ 02-Nov-2020
Thermal Episode of Chondrule Formation
⏲ 3 min 34 sec ✓ 08-May-2019
Nov 22 DLL Trades Productivity with Mafic
⏲ 34 sec ✓ 03-Nov-2022
Mineral Crystallisation in Chondrules (Di - An - Fo including binary systems)
⏲ 4 min 58 sec ✓ 09-May-2019
The Wedding Market - Campaign 2019
⏲ 78 sec ✓ 30-Aug-2019
Shock Wave Model of Chondrule Formation
⏲ 2 min 72 sec ✓ 07-May-2020
ERTA ALE - AFAR - ETHIOPIA
⏲ 1 min 70 sec ✓ 19-Nov-2022
Mafic FAIRPAY introduction
⏲ 4 min 30 sec ✓ 25-May-2022
French in Philippines visits Gk Enchanted farm
⏲ 60 sec ✓ 31-Mar-2017
Cao Bang - A Base To Exlore Beautiful Nature In Vietnam
⏲ 2 min 14 sec ✓ 29-Jan-2021
Mafic - Safeguard
⏲ 1 min 13 sec ✓ 07-Feb-2023
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_mineral-crystallisation-in-chondrules-an-sio2-fo-including-binary-systems.webp "Chondrules are mafic, magmatic systems. Chondrule crystallisation can be described in e.g., the petrologic ternary phase diagram Forsterite-Anorthite-Quartz. In brief, and only the most typical path: most chondrules start deep in the forsterite primary phase field. A melt then develops towards the peritectic line, where the peritectic reaction olivine + silica produces pyroxene from the olivine over-saturated melt. The melt develops along the peritectic line during this reaction and towards the")
_hiclip-the-color-palette-of-nilosyrtis-mensae.webp "The region of Mars north of the Syrtis Major volcanics and the Isidis impact basin has well-exposed bedrock with diverse compositions. These regions are dark so the colors aren't well seen except with a sensitive imager like HiRISE and special processing. nnThe blue and green colors are generally due to mafic (magnesium and iron rich) minerals that are not altered by water, while the warmer colors are due to altered minerals like clays. The structure in this scene is quite complex from a combina")
_thermal-episode-of-chondrule-formation.webp "Most chondrules contain large, often porphyritic olivine and pyroxene grains, sitting in a glassy to fine-crystalline, Ca,Al-rich, often feldspar-like material. This material is called ›mesostasis‹ and its glassy to fine-crystalline structure is one of the strongest arguments that chondrules were once molten and cooled quickly, or have been even quenched. Another argument for quick cooling are unexpected high concentrations of volatile elements such as Na, that should have been evaporated at")
_nov-22-dll-trades-productivity-with-mafic.webp "Nov 22 DLL Trades Productivity with Mafic from mafic")
_mineral-crystallisation-in-chondrules-di-an-fo-including-binary-systems.webp "Chondrules are mafic, magmatic systems. Chondrule crystallisation can be described in e.g., the petrologic ternary phase diagram Diopside-Anorthite-Forsterite. In brief, and only the most typical path: most chondrules start deep in the forsterite primary phase field. A melt then develops towards either the Fo+An or Fo+Di cotectic line, from where on the respective two minerals crystallise unit reaching the eutectic point. There, the 3 phases Fo+Di+An crystallise together until all melt is consum")
_the-wedding-market-campaign-2019.webp "Directed bynThe Wedding MarketnnFilmed & EditednalCuadrado VideographynnLocationnMafic SpacennInterpreted bynJulie LeblondnnMake up & Hair ArtistnEl Baul de RuthnnWedding DressnL’arca BarcelonannCake Designer nSweet Events by Jess")
_shock-wave-model-of-chondrule-formation.webp "Chondrule precursors likely consisted of up to millions of µm-sized dust grains. Millions of such chondrule precursors likely existed, surrounded by a reducing gas. A shock wave travelling through such a gaseous chondrule precursor regions compresses the gas and accelerates it and everything within it in its travelling direction. The massive compression and friction of the materials raises the temperature shortly behind the shock front within minutes or less from a few hundred K to more than 20")
_erta-ale-afar-ethiopia.webp "Erta Ale - Afar - Ethiopia 2022nnErta Ale (or Ertale or Irta'ale; Amharic: ኤርታሌ) is a continuously active basaltic shield volcano in the Afar Region of northeastern Ethiopia. It is situated in the Afar Depression, a barren desert area. Erta Ale is the most active volcano in Ethiopia.nnGeologynErta Ale is 613 metres (2,011 ft) high, with one or sometimes two active lava lakes at the summit which occasionally overflow on the south side of the volcano. It is notable for holding the longest-")
_mafic-fairpay-introduction.webp "Mafic FAIRPAY introduction from mafic")
_french-in-philippines-visits-gk-enchanted-farm.webp "the French community in Manila discovers the beauty of the land and the mafic of the rural bright people of Gawad Kalinga and Enchanted farm")
_cao-bang-a-base-to-exlore-beautiful-nature-in-vietnam.webp "The Cao Bang UNESCO Global Geopark in a mountainous area in the northeast of the country. Geologically Cao Bang Geopark can be divided into two distinct parts by the so-called Cao Bang-Tien Yen deep-seated active fault. The eastern part of the area is composed of Palaeozoic limestones. The western part features sedimentary rocks, pillow basalts, ultra-mafic and granitic intrusions rich in minerals and hydrothermal alterations. The majority of its population belongs to one of nine different ethni")
_mafic-safeguard.webp "Mafic - Safeguard from mafic")
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