12035 (68) - Olivine basalt
Collection:
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Fact sheet

12035 (68) - Olivine basalt

12035 is a friable, vuggy, micro-gabbro with euhedral to subhedral chrome spinel and olivine, and subhedral to anhedral clinopyroxene enclosed by poikilitic plagioclase. Interstitial ilmenite tends to be anhedral. The sample has also been described as a coarse olivine-rich (30%) gabbro with euhedral clinopyroxene, subhedral olivine and large plagioclase grains. The olivine is relatively iron rich, hence it is not a simple cumulate for the other olivine basalts, but rather the olivine has re-equilibrated with the liquid. Olivine phenocrysts in 12035 contains melt inclusions. Plagioclase crystals (~1 mm) are larger than those in other Apollo 12 olivine basalts.

The sample weighed 71 grams before analysis and is 3.2 billion years old (Rb-Sr).

The large plagioclase crystals in this sample appear to contain many colourless spherical inclusions. These are probably artifacts introduced as the embedding resin changed over time. The thin section is nearly 50 years old.

Further details of this and other Apollo samples are here: http://curator.jsc.nasa.gov/lunar/

About this collection

Apollo 12 returned 34 kilograms of samples, including 45 rocks, samples of lunar 'soil', and several core tubes that included material from as much as 40 centimetres below the lunar surface.

Apollo 12 rocks were almost all basalts, with only two breccias in the returned samples. The basalts at the Apollo 12 site formed 3.1 to 3.3 billion years ago, roughly 500 million years later than the Apollo 11 basalts. Overall, there is much less of the element titanium in the Apollo 12 samples than in the Apollo 11 samples, which explains the more reddish colour of this region. The differences in age and chemical composition between the Apollo 11 and Apollo 12 samples demonstrate that mare volcanism did not occur as a single, Moon-wide melting event.

Apollo 12 was launched on 14 November 1969.

Sample details

Collection: Apollo 12
Type
igneous
Rock-forming mineral
olivine
pyroxene
plagioclase
feldspar
Accessory minerals
ilmenite
chrome-spinel
troilite
metallic iron
Category guide  
Category Guide
Title
Refers to any word or phrase that appears in the individual rock names. Names are generally descriptive; they allow users to search for broad terms like ‘granite’ as well as more specific names such as ‘breccia’. However, the adjacent descriptions of the specimens captures a wider range of general words and phrases and is a more powerful search tool.
Description
Refers to any word or phrase that appears anywhere in the descriptions of the specimens
Accessory minerals
Minerals that occur in very low abundance in a rock. They are usually not visible with the naked eye and contribute perhapssver, they often dominate the rare elements such as platinum group metals.
Rock-forming minerals
Minerals that make up the bulk of all rock samples and are also the ones used in rock classi?cation.
Timescale
Selecting one or more period, for example 'Jurassic'.
Theme
A term used to group together related samples that are not already gathered into a single Collection. For instance, there is a ‘SW England granites’ theme that includes such rock types as granite, hydrothermal breccia, skarn and vein samples.
Category
A general term used to label a rock sample. It is a useful way of grouping similar samples throughout a collection. Category names are often, but not exclusively, common rock names (e.g. granite, basalt, dolerite, gabbro, greisen, skarn, gneiss, amphibolite, limestone, sandstone).
Owner
The owner of the sample that appears in the collection. For example, NASA owns all the samples that appear in the Moon Rocks collection
We would like to thank the following for the use of this sample: