TABLE 10. Meteorites from the Sahara, locations unknown.

Name Latitude� Longitude� Mass (g) Pcs Class Shock WG Fa Fs Comments

Sahara
98058 z+0�10'55" w+0�31'23" 681 1 H5 S3 2 19.6 16.5 sv
98276 z+0�08'52" w+0�28'50" 93 1 L6 S6 2 25.6 22.2 sv, rw
98429 z+0�08'48" w+0�28'48" 137 1 L6 S4 2/3 26.1 22.3 sv
98473 z+0�08'50" w+0�28'31" 68 1 L6 S3 2 25.7 21.9 br, sv
98639 z+0�08'54" w+0�28'31" 300 1 H4 S3 3 20.9 18.9 close to L4
98660 z+0�09'23" w+0�28'17" 141 1 L3-6 S3 1/2 22.9 19.6 br, sv
ranges: 2-32 5-26
98645 z+0�09'32" w+0�28'21" 51 1 H3 S3 1/2 19.1 15.7
ranges: 10-24 5-24
98683 z+0�09'26" w+0�28'10" 361 1 L3 S3 2 21.1 12.1
ranges: 5-29 1-23
98691 z+0�09'35" w+0�28'05" 16 1 L3 S3 2/3 23.2 15.2
ranges: 6-33 2-23
98748 z+0�09'37" w+0�28'05" 439 2 H3-6 S3 1 17.9 16.8
ranges: 0-27 7-19
98782 z+0�09'33" w+0�28'33" 47 1 L3 S4 1/2 25.4 16.1
ranges: 6-36 5-29
99037 z+0�09'56" w+0�29'18" 365 1 H6 S2 1 20.1 17.7 br, mv
99076 z+0�09'48" w+0�29'19" 62 1 How� ~40 24-34 (diog. frags)
50-57 (euc. frags)
99314 z+0�09'33" w+0�29'27" 56.5 1 How? 25-31 (diog. frags)
50-60 (euc. frags)
99082 z+0�03'35" w+0�31'03" 135 1 H4/5 S4 1/2 17.7 16.6
99099 z+0�03'36" w+0�30'50" 267 1 LL6 31.5 25.9 br
99159 z+0�03'37" w+0�30'54" 1023 1 LL3 27.8 17.7
�9.4 �10.4
99339 z+0�09'32" w+0�28'26" 32.4 1 LL(L)3 S2 3 14.4 13.7 subtype <3.5
�8.9 �10.4
99456 z+0�10'26" w+0�30'44" 62 1 E6& S2 2 <0.5
99502 z+0�13'45" w+0�32'10" 481 2 LL6 S3 4 32 26.5 br, sv
99527 z+0�09'16" w+0�28'54" 19 1 R5 S3 4 39.9 sv
99531 z+0�09'18" w+0�28'57 31 1 R3-5 S3 3/4 40.4 br, sv
2-42 (uneq. clasts)
99537 z+0�09'19" w+0�28'59" 27 1 R3-6 S3 3/4 40.0 br, sv
3-42 (uneq. clasts)
99544 z+0�08'45" w+0�29'28" 1360 1 CO3* S2 2 0-60
99555 z+0�13'53" w+0�32'01" 2710 1 Angrite#

Abbreviations: br = breccia; diog = diogenite; euc = eucrite; mv = metal veins; rw = ringwoodite; sv = shock veins; uneq = unequilibrated.
The geographic coordinates of these meteorites have not been disclosed by the finder. Listed are the offsets relative to a secret origin at (w�W longitude, z�N latitude, where w and z are integers that are not the same as x and y in Table 7 of Met. Bull. 82).
Plagioclase An63-93 and SiO2 occur in the diogenitic fraction.
?Plagioclase An86-93 occurs in the diogenitic fraction.
&Contains no relict chondrules.
*Fa and Fs mainly <5 mol% in chondrule minerals
#Contains anorthite, fassaite, olivine and kirschsteinite; see Bischoff et al. (2000).