top of page

Shergottites

page top

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2018

Mass

1150 g

[Museum Collection]

(1) 0.51g  

History: Purportedly found in Algeria and purchased by Mohamed Brahim Sueilem in August 2018 from a dealer in Bordj Badji Mokhtar, Algeria. Physical characteristics: The material (total weight 1150 g) comprises multiple broken fragments, some with adhering black fusion crust. The friable pieces are pale green in color and contain white plagioclase but no evident maskelynite. Petrography: (A. Irving and S. Kuehner, UWS) This fresh specimen has an orthocumulate texture with ~15 vol.% lath-like, birefringent plagioclase occurring interstitially to more abundant and coarser grained (0.2-1.6 mm, mean 0.7 mm) mafic silicate grains (unzoned olivine and patchily zoned low-Ca and high-Ca clinopyroxene with very limited compositional variation). Accessory phases include Mg-merrillite, chlorapatite, ilmenite, Ti-rich chromite, Cr-rich chromite and pyrrhotite (some associated with minor pentlandite). Levels of shock are judged to be low, based on the absence of optical effects in plagioclase and the complete lack of any conversion to maskelynite; the presence of widespread microcracks in mafic silicates is the only clear evidence of shock. Geochemistry: Olivine (Fa32.7-34.3, FeO/MnO = 47-48, N = 4), pigeonite (Fs25.0-30.4Wo5.5-10.0, FeO/MnO = 28-30, N = 4), subcalcic augite (Fs17.1-18.1Wo32.7-32.4, FeO/MnO = 23-25, N = 2), aluminous augite inclusion in olivine (Fs17.1Wo39.5, FeO/MnO = 28, TiO2 = 1.1 wt.%, Al2O3 = 6.2 wt.%), plagioclase (An43.0-57.8Or2.4-1.3, N = 3). Oxygen isotopes (K. Ziegler, UNM): analyses of acid-washed subsamples by laser fluorination gave, respectively, δ17O 2.907, 2.635, 2.808; δ18O 5.092, 4.620, 4.875; Δ17O 0.218, 0.195, 0.234 per mil. Classification: Martian (shergottite, olivine gabbroic, orthocumulate, low shock). Specimens: 22.4 g including one polished thin section at UWB; remainder held jointly by Naji Ben Faraji and Mohamed Brahim Sueilem.

NWA12241
NWA12262

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2018

Mass

3.29 kg

[Museum Collection]

(1) 2.79g   (2) 1.26g

History: Purchased in Ouarzazate, Morocco by Mohamed Aid in July 2018. Petrography: (A. Irving and S. Kuehner, UWS; P. Carpenter, WUSL) Medium-grained with diabasic texture and some small, dark glassy shock melt pockets. Composed predominantly of zoned clinopyroxene and maskelynite with accessory fine grained intergrowths of hedenbergite+fayalite+silica, Fe-Ti oxide (finely exsolved), merrillite and pyrrhotite. Geochemistry: Subcalcic augite (Fs28.5-30.6Wo28.2-23.7, FeO/MnO = 30, N = 2), pigeonite (Fs41.3Wo15.5, FeO/MnO = 31), ferropigeonite (Fs71.1-83.4Wo17.1-11.3, FeO/MnO = 38-45, N = 4), maskelynite (An50.9-52.1Or2.1, N = 2). Classification: Martian (shergottite, diabasic) Specimens: 26.3 g including one polished thin section at UWB; remainder with Aaronson.

NWA12269

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2018

Mass

1679 g

[Museum Collection]

(1) 7.02g   (2) 1.34g

History: Purchased in Ouarzazate, Morocco by Mohamed Aid in July 2018. Petrography: (A. Irving and S. Kuehner, UWS; P. Carpenter, WUSL) Relatively fine grained with intersertal texture. Composed predominantly of zoned clinopyroxene and maskelynite (some exhibiting a curved, narrow lath-like habit) with accessory fine grained intergrowths of hedenbergite+fayalite+silica, Fe-Ti oxides, merrillite and pyrrhotite. Geochemistry: Subcalcic augite (Fs24.8-41.8Wo31.4-24.3, FeO/MnO = 30-33, N = 3), ferropigeonite (Fs66.9-73.0Wo16.6-16.5, FeO/MnO = 41-43, N = 2), maskelynite (An51.9-53.1Or1.3-1.2, N = 2). Classification: Martian (shergottite, fine-intersertal) Specimens: 20.5 g including one polished thin section at UWB; remainder with Mr. Aaronson.

NWA12594

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2018

Mass

150 g

[Museum Collection]

(1) 9.59g   (2) 0.97g   (3) 0.82g

History: Found in Algeria in 2018 and purchased from a Moroccan dealer by Huapei Wang in 2018 Physical characteristics: These stones are (partially) covered by black fusion crust and appear to be very fresh and unaltered. Numerous vesicles are seen in the fusion crust. The interior is composed of yellow green grains with interstitial pale gray grains. Petrography: The rock has a medium-grained subophitic texture. It consists of elongated prismatic pyroxene (up to 1.5 mm in length) and lath-like plagioclase (up to 1.8 mm in length), with accessory titanomagnetite, ilmenite, silica polymorph, merrillite, pyrrhotite, fayalite. Pyroxenes show patchy zoning from Mg-rich core to Mg-poor rim, with irregular boundaries. Ilmenite occurs as thin lamellae intergrown with titanomagnetite. Geochemistry: Pyroxenes are zoned from augite cores (En45.3Wo25.6, FeO/MnO = 28.5) and pigeonite cores (En40.3Wo19.6 FeO/MnO = 32.3) to ferropigeonite rims (En8.4Wo14.5 FeO/MnO = 41.1). Plagioclase is characterized by homogeneous compositions of An52 Or1.4. Titanomagnetite (TiO2 29.4 wt%, FeO 65.5 wt%, Al2O3 1.3 wt%); ilmenite (TiO2 48.9 wt%, FeO 49.8 wt%).

NWA13327

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2020

Mass

346 g

[Museum Collection]

(1)20.529g  (2)10.515g  (3)4.461g  (4)3.613g
(5)3.609g    (6)3.178g    (7)3.144g  (8)2.531g
(9)2.445g    (10)1.982g  (11)1.860g  (12)1.562g
(13)1.544g  (14)1.468g  (15)1.408g  (16)1.399g
(17)1.288g  (18)1.275g  (19)1.260g  (20)1.110g
(21)1.024g  (22)0.879g  (23)0.858g  (24)0.853g
(25)0.795g  (26)0.730g  (27)0.717g  (28)0.711g
(29)0.699g  (30)0.608g  (31)0.566g (32)0.517g
(33)0.497g  (34)0.462g  (35)0.451g  (36)0.446g
(37)0.424g

History: Purchased by Eric Twelker in February 2020 from a Moroccan dealer at the Tucson Gem and Mineral Show. Petrography: (A. Irving, UWS and P. Carpenter, WUSL) Diabasic texture (mean grainsize ~0.8 mm). Composed predominantly of prismatic grains of zoned clinopyroxene and lath-like maskelynite together with accessory silica polymorph, merrillite, chlorapatite, Cr-Mn-bearing ulvöspinel, ilmenite, pyrrhotite and baddeleyite. Minor secondary calcite is present. Geochemistry: Subcalcic augite (Fs20.1-27.3Wo29.1-35.4, FeO/MnO = 19-34 , N = 5), ferroan subcalcic augite rim (Fs45.1Wo30.7, FeO/MnO = 36), ferroan pigeonite rims (Fs53.9-61.3Wo13.4-15.7, FeO/MnO = 36-37, N = 3), maskelynite (An53.4-55.7Or1.4-0.9, N = 4). Classification: Shergottite (diabasic). Specimens: 20.5 g plus one polished thin section at UWB; remainder with Mr. E. Twelker.

NWA13367

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2020

Mass

249 g

[Museum Collection]

(1) 5.50g

History: Purchased from a Moroccan dealer in April 2020. Physical characteristics: Single stone, fusion crust, saw cuts reveals an ultramafic cumulate rock with ophitic to poikilitic textures with mm-size pale yellow and dark gray grains. Petrography: (C. Agee, UNM) Microprobe examination shows approximately 50% olivine, 40% pyroxene, and 10-5% maskelynite. Two distinct pyroxene trends are present 1) Mg-rich low calcium pyroxene trending to slightly more Fe-rich pigeonite, 2) Mg-rich augite trending to more Ca-rich augite. Ilmenite, spinel, Fe-sulfide, and merrillite are minor ubiquitous phases. Geochemistry: (C. Agee, UNM) Olivine Fa34.6±2.0, Fe/Mn=49±2, n=10; low Ca-pyroxene Fs22.5±0.5Wo4.7±0.7, Fe/Mn=29±2, n=6; augite Fs17.2±0.9Wo32.4±2.8, Fe/Mn=24±1, n=4; maskelynite An52.9±2.3Ab46.0±2.2Or1.1±0.2, n=4, fusion crust SiO2=46.5±0.6, TiO2=0.9±0.1, Al2O3=8.6±3.5, Cr2O3=0.7±0.1, MgO=18.0±3.5, FeO=15.3±0.5, MnO=0.4±0.1, Na2O=1.4±0.5 (all wt%), n=2. Classification: Martian peridotitic shergottite. Macroscopic textural appearance similar to NWA 1950 and ALHA77005. Paired with NWA 13250. Specimens: 20 g on deposit at UNM, Marcin Cimala holds the main mass.

NWA15876

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2023

Mass

339 g

[Museum Collection]

(1) 5.25g   (2) 2.57g 

History: The meteorite was purchased from a meteorite dealer in Morocco. Physical characteristics: Grayish to dark greenish fragments with patches of black fusion crust. Petrography: The meteorite shows a poikilitic texture of up to 3 mm sized pyroxenes enclosing rounded to subrounded olivines that frequently contain trapped melt inclusions. Feldspar is a minor component and has completely been transformed to maskelynite. Accessory minerals include chomite, FeS and FeNiS. Contains glassy to finely recrystallized shock melt pocket. Geochemistry: olivine: Fa27.8±0.7 (Fa26.8-28.4, FeO/MnO=44±1, n=10); orthopyroxene: Fs18.7±0.3Wo2.4±0.1 (Fs18.3-19.5Wo2.3-2.6, FeO/MnO=27±2, n=10); pigeonite: Fs24.6±1.5Wo10.6±2.3 (Fs20.4-26.6Wo7.1-13.7, FeO/MnO=26±1, n=10); maskelynite (An53.2-56.3Ab42.4-45.4Or1.3-1.5, n=10) Classification: Martian meteorite (shergottite); likely paired with NWA 10961

NWA16127

Name

*click on the Name for more information

Structure Class

achondrites

Chemical Class

Martian (shergottite)

Country

Year found

2023

Mass

200 g

[Museum Collection]

(1) 2.21g   (2) 1.54g 

History: Purchased by Ruben Garcia from a Moroccan meteorite dealer. Physical characteristics: Sandblasted exterior lacking fusion crust. Broken surface reveals a mix of gray-brown pyroxene grains and shiny maskelynite grains. Petrography: (C. Agee and M. Spilde, UNM) The two major phases in this meteorite are clinopyroxene and maskelynite. Ubiquitous titanomagnetite was observed throughout. The clinopyroxene has a modal abundance of approximately 50%, with significant core to rim zoning observed in backscatter electron images indicating an igneous crystallization trend with Mg-rich augite and pigeonite cores, rimmed with ferropigeonite. Clinopyroxene average grain size is approximately 400-700 μm. Maskelynite has modal abundance of approximately 40%. Geochemistry: (M. Spilde, UNM) Clinopyroxene Fs46.2±15.0Wo25.5±7.5, Fe/Mn=37±4, n=36; maskelynite An53.9±2.0Ab45.2±2.0Or0.9±0.0, n=4. Classification: Evolved pyroxene-phyric basalt, clinopyroxene compositional zoning trends are similar to QUE 94201. Specimens: 20.2 g on deposit at UNM, Ruben Garcia holds the main mass.

bottom of page