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Post Info TOPIC: Tambakwatu meteorite


L

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RE: Tambakwatu meteorite
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Title: The Tambakwatu chondrite
Authors: Fredriksson, K.; Miller, J.; Nelen, J.; Darsa, S.

The texture and mineralogy of a meteorite that fell to earth on February 14, 1975, near the village of Tambakwatu (Indonesia) are analyzed. Modal analysis by point counting one thin section (a total of approximately 1 sq cm) shows that Tambakwatu is about 87 wt % silicates, 8 wt % metal, 4.5 wt % troilite, and 0.5 wt % chromite. It is noted that the chondrules, most of which are barred or porphyritic, are generally fragmented with barely distinguishable boundaries. A table giving the composition of the meteorite is included. On the basis of classical nomenclature, Tabakwatu is defined as a veined, intermediate hypersthene chondrite (Cia). According to the classification scheme proposed by Van Schmus and Wood (1967), the meteorite is an L6 chondrite.

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Name: TAMBAKWATU
Place of fall: Near the village of Tambakwatu, Java, Indonesia.
7°45'S., 112°46'E., approx.
Date of fall: February 14, 1975, before midnight.
Class and type: Stone. Olivine-hypersthene chondrite (L6). Olivine Fa23.8, pyrox­ene Fs20.4.
Number of individual specimens: 1
Total weight: 10.5 kg.
Circumstances of fall: Seen to fall in the countryside of the Purwosari district. Recovered later by the Jakarta Planetarium.

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L

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The Tambakwatu (L6) meteorite fell in Jawa Timur, Indonesia, on the 14th February, 1975.
A total mass of 10.5 kg was recovered.

7° 45'S, 112° 46'E



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