nya dating resulterar från analysen av isotoper av dodelplombet som finns i ett prov av anorthosite, den äldsta stenen av månskorpan ( FAN, ferroanortositt ).

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Revision 2: submission to American Mineralogist. Spinel-Anorthosites on the Moon: Impact Melt Origins Suggested by Enthalpy Constraints Allan H. Treiman1, Michael J. Kulis2, and Allen F. Glazner3 1 Lunar and Planetary Institute – Universities Space Research Association, 3600 Bay Area Boulevard, Houston, TX 77058. treiman@lpi.usra.edu

Geochimica et Cosmochimica Acta Supplements 1, 965-988. ). Here we show  While Apollo astronauts returned with 382 kg of Moon rocks, not one milligram is primarily lunar anorthosite with approximately 90-95% plagioclase with minor  5 May 2020 The Apollo astronauts brought back samples of anorthosite from the Moon. These samples are important in helping scientists understand the  3 Oct 2018 Anorthosite is an intrusive igneous rock composed mainly of silicates of volatile materials in Earth anorthosite and Moon anorthosite allow us  This rock is NOT from the Moon but it is one of Earth's best equivalent to the " Genesis Rock" brought back by Apollo 15. Great medium-sized hand specimen. 1 Feb 2017 The only known larger anorthosite deposit is on the moon. universe: Hudson Resources' White Mountain project in Greenland and the moon.

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As rare as anorthosite is on our planet, it is extremely abundant on the Moon, being the primary constituent of the lunar crust and the bright-colored lunar highlands. [1] We present a new global survey of the purest anorthosite (PAN) rock using the Spectral Profiler onboard Kaguya.

Mineralogical Magazine 80 5 Lunar basalt chronology, mantle differentiation and Lithos , The source of Proterozoic anorthosite and rapakivi granite 

This white rock is composed almost entirely of crystals of one mineral, feldspar. Rocks like this make up much of the Highlands of the Moon, where feldspar produces the light color. Shortly after material gathered together to form the Moon, the outer Moon melted. 2014-09-01 · The formation of pure anorthosite on the Moon 1.

Earth's Moon can be looked upon as an enormous Earth-orbiting Space Pieters et al (2001) used Clementine UVVIS data to distinguish between anorthosite,.

Anorthosite moon

Allard Lake, Southern Quebec. 3. Ukraine of USSR. 4. The formation of lunar anorthosites is discussed, and gabbro-anorthosite inclusions in island-arc volcanics are compared with lunar-highland rocks. The physical-chemical aspects of anorthosite formation are investigated, and the early stages of the evolution of the earth and moon are examined on the basis of a comparison of terrestrial and lunar anorthosites.

Anorthosite moon

All PAN sites are associated with huge impact structures with diameters larger than 100 km. Based on the global distributions of PAN … Select Page. anorthosite on the moon. by | Jan 17, 2021 | Uncategorized | 0 comments | Jan 17, 2021 | Uncategorized | 0 comments Anorthosite was prominently represented in rock samples brought back from the Moon, and is important in investigations of Mars, Venus, and meteorites. Anorthosite from southern Finland.
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Anorthosite moon

The most common  At 4.5 billion years old, this anorthosite is approximately the same age as the Moon itself.

Mineralogical Magazine 80 5 Lunar basalt chronology, mantle differentiation and Lithos , The source of Proterozoic anorthosite and rapakivi granite  Mineralogical Magazine 80 5 Lunar basalt chronology, mantle differentiation and Lithos , The source of Proterozoic anorthosite and rapakivi granite  Mineralogical Magazine 80 5 Lunar basalt chronology, mantle differentiation and Lithos , The source of Proterozoic anorthosite and rapakivi granite  Mineralogical Magazine 80 5 Lunar basalt chronology, mantle differentiation and Lithos , The source of Proterozoic anorthosite and rapakivi granite  It is built on a 130-foot (40 m) sheer cliff of anorthosite. The lighthouse was first lit on July 31, 1910.
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Anorthosite moon




Some clasts are basalt from lunar lowlands.The anorthosite clasts come from the lunar… Kaitlin HarrisonMinerals · MPOD 120605 from Tucson Meteorites 

Therefore, it is important to determine the distribution and modes of occurrence of anorthosite on the lunar surface. We have been conducting remote sensing studies of occurrence of anorthosite on the Moon r equires a global ma gma body, referred t o as the 70 lunar magma ocean (LMO) (Yamamoto et al., 2012). The “giant impact” scenario ha s 71 Anorthosite .


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Anorthosite . This white rock is composed almost entirely of crystals of one mineral, feldspar. Rocks like this make up much of the Highlands of the Moon, where feldspar produces the light color. Shortly after material gathered together to form the Moon, the outer Moon melted.

Fortunately, the rock can also be found on Earth. The giant impact hypothesis for the origin of the Moon points to the creation of a hot, young Moon, likely with a global magma ocean. Such a magma ocean would produce a flotation crust of plagioclase crystals, or an anorthositic crust. Early calculations of the expected anorthosite content of the lunar highlands crust did not match initial measurements of Apollo samples, and more recently have The anorthosite body was formed as an accumulation of plagioclase crystals at the bottom of the magma chamber. Anorthosite can vary widely in color.