Thin-section making and observation from the field excursion in Kanchanaburi, Thailand 2024  Yoshio Okamoto 15 Feb. 2024

1. Making thin-sections

I have some rock samples from the field excursion at Kanchanaburi, this year.
Therefore, I am trying to make thin-sections at first.
The first samples are sapphire bearing basalt at Khao Lum Thom (Bo Phloi, Kanchanaburi).


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from http://seagull.stars.ne.jp/2024_MUKA/MUKA_Part_2.html
REf. about this rock is https://www.geo.sc.chula.ac.th/BEST/volume3/Number1/4_BEST_3_1_004_Sutthirat%20et%20al.pdf


Ref. My thin-section pages:  http://yossi-okamoto.net/Thin-Sections/index.html
Ref.Poster Okamoto(2021): http://www.yossi-okamoto.net/conference/EER2021_Poster.pdf



Cut a sapphire bearing basalt at Khao Lun Thom (Bo Phloi, Kanchanaburi), Thickness is around 1 mm. Click on video.
Grind on a #180 and #320 diamond plates placed on a kitchen knife sharpener.Click on video. This video shows #320 grinding.

Hand grinding #800 carborundum+ water on a thick glass plate. It is most important process of my thin-section making. 
The section color is thinning. When the thickness about the section reaches 0.03mm, A short grinding using #1500 alumdum is the final stage.

Check the interference color of plagioclases reaches grey or white. It is the sign of good thickness. After #1500, a cover glass is fix by UV curable adhesive.   Labeled thin section of LKT basalt.

2. Observing thin-sections
 
 Typical basalt texture with olivine phenocrysts. However there are some amygdal or xenolith like structures.
I am not an expert of petrology, so only I can recognize some plagioclases, olivines and clino-pyroxenes. If you have any comment, please let me know via Line or email. View area is 8.5 x 5.7mm.

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The same sample above making under XPL. There is an amygdal or xenolith is seen. This seems to be a gabbro composition. The same sample above making under PPL. Some matrix are altered brownish minerals.
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Another amygdal or xenolith. The long and thin plagioclases look somewhat serpentine. Strong interference color minerals are clino-pyroxenes. It is difficult for me to distinguish this is an amygdal or tiny xenolith.
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Another matix part of the second sample. The left center phenocryst is an olivine.
Phenocryst olivines are not altered by Iddingsite.


Click the movie start.
Click the movie start.
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I forgot to put a scale. This scale is in 0.5mm increments. A poikilitic texture of pyroxenes is clear in the central xenocryst.
An opaque crystal in the center upward.


My thin-section microscope: LAOWA 25mm High-Resolution Close up Lens with Canon EOS M.
The polarized unit is also my hand-made.
LAOWA 25mm High-Resolution Close up Lens: this is the best lens for thin-section photography in my experience.
http://www.yossi-okamoto.net/conference/EER2021_Poster.pdf




















  
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