编号 84593177

已不存在
Tazizilet 002 - 陨石球粒陨石 OC4 熔融角砾岩 - 超薄切片! - 高度: 86 mm - 宽度: 75 mm - 29.99 g
竞投已结束
2天前

Tazizilet 002 - 陨石球粒陨石 OC4 熔融角砾岩 - 超薄切片! - 高度: 86 mm - 宽度: 75 mm - 29.99 g

Complete slice of Tazizilet 002 : unique chondritic melt material OC4 showing nice metal inclusions and encapsulated chondrules Size : 86*75*1.5-2 mm Wight : 29.99 gr Check metbull link for detail and history : https://www.lpi.usra.edu/meteor/metbull.php?code=80862 Writeup from MB 112: Tazizilet 002 17.47662662, 9.545471183 Agadez, Niger Find: 2022 Oct Classification: Ordinary chondrite (type 4, melt breccia) History: Two individual masses of 1173 and 1089 g were found in October 2022 by gold prospectors using a metal detector in the vicinity of Mount Amzeguer, Niger. In November 2022, both specimens were acquired by Sylvain Leroux in Agadez, Niger, directly from the finder Ahmat, and kindly conveyed by Hassane Ousmane. Material for classification was send to A. Greshake (MNB) and H. Goethals and T. Leduc (RBINS). Physical characteristics: Two dark brownish rocks lacking fusion crust. Petrography: (A. Greshake, MNB; H. Goethals and T. Leduc, RBINS) Metal-rich chondritic breccia composed of cm sized mostly angular chondritic clasts separated from each other by partially melted and finely recrystallized portions containing abundant thin metal veins. Chondritic regions contain well-defined, mostly flattened and separated chondrules (apparent diameter about 600 µm) of a great variety of types including PO, PP, POP, GOP, RP, and C. Predominant chondrule minerals are forsteritic olivine, magnesian orthopyroxene typically overgrown by Ca-rich pyroxene rims plus sodic plagioclase. Interchondrule matrix contains abundant Cl-apatite, chromite, FeNi metal, and troilite. No secondary plagioclase detected. FeNi metal is significantly more abundant in melt rock regions compared to chondritic clasts. Geochemistry: olivine: Fa8.4±0.1 (Fa8.3-8.7, FeO/MnO=16-19, n=10), orthopyroxene: Fs8.8±0.3Wo0.6±0.1 (Fs8.4-9.0Wo0.8-1.1, FeO/MnO=10-13, n=10); augite: Fs4.6±0.3Wo38.6±1.4 (Fs3.9-5.0Wo36.4-41.5, FeO/MnO=5-9, n=10) Classification: OC4-melt breccia. Likely related to Northwest Africa 15468 and pairs. Specimens: 69 g including one polished thin section at MNB; two polished discs at RBINS; remainder held by Mr. Sylvain Leroux Cut and polished by La Pierrerie de l'Aïr Shipped by La Pierrerie de l'Aïr, from Belgium. Tracking and insurance included in shipping costs. I'm a GMA member #G0106

编号 84593177

已不存在
Tazizilet 002 - 陨石球粒陨石 OC4 熔融角砾岩 - 超薄切片! - 高度: 86 mm - 宽度: 75 mm - 29.99 g

Tazizilet 002 - 陨石球粒陨石 OC4 熔融角砾岩 - 超薄切片! - 高度: 86 mm - 宽度: 75 mm - 29.99 g

Complete slice of Tazizilet 002 : unique chondritic melt material OC4 showing nice metal inclusions and encapsulated chondrules

Size : 86*75*1.5-2 mm
Wight : 29.99 gr

Check metbull link for detail and history : https://www.lpi.usra.edu/meteor/metbull.php?code=80862

Writeup from MB 112:
Tazizilet 002 17.47662662, 9.545471183
Agadez, Niger
Find: 2022 Oct
Classification: Ordinary chondrite (type 4, melt breccia)
History: Two individual masses of 1173 and 1089 g were found in October 2022 by gold prospectors using a metal detector in the vicinity of Mount Amzeguer, Niger. In November 2022, both specimens were acquired by Sylvain Leroux in Agadez, Niger, directly from the finder Ahmat, and kindly conveyed by Hassane Ousmane. Material for classification was send to A. Greshake (MNB) and H. Goethals and T. Leduc (RBINS).
Physical characteristics: Two dark brownish rocks lacking fusion crust.
Petrography: (A. Greshake, MNB; H. Goethals and T. Leduc, RBINS) Metal-rich chondritic breccia composed of cm sized mostly angular chondritic clasts separated from each other by partially melted and finely recrystallized portions containing abundant thin metal veins. Chondritic regions contain well-defined, mostly flattened and separated chondrules (apparent diameter about 600 µm) of a great variety of types including PO, PP, POP, GOP, RP, and C. Predominant chondrule minerals are forsteritic olivine, magnesian orthopyroxene typically overgrown by Ca-rich pyroxene rims plus sodic plagioclase. Interchondrule matrix contains abundant Cl-apatite, chromite, FeNi metal, and troilite. No secondary plagioclase detected. FeNi metal is significantly more abundant in melt rock regions compared to chondritic clasts.
Geochemistry: olivine: Fa8.4±0.1 (Fa8.3-8.7, FeO/MnO=16-19, n=10), orthopyroxene: Fs8.8±0.3Wo0.6±0.1 (Fs8.4-9.0Wo0.8-1.1, FeO/MnO=10-13, n=10); augite: Fs4.6±0.3Wo38.6±1.4 (Fs3.9-5.0Wo36.4-41.5, FeO/MnO=5-9, n=10)
Classification: OC4-melt breccia. Likely related to Northwest Africa 15468 and pairs.
Specimens: 69 g including one polished thin section at MNB; two polished discs at RBINS; remainder held by Mr. Sylvain Leroux

Cut and polished by La Pierrerie de l'Aïr
Shipped by La Pierrerie de l'Aïr, from Belgium.
Tracking and insurance included in shipping costs.
I'm a GMA member #G0106

设置搜索提醒
设置搜索提醒,以便在有新匹配项目时随时收到通知。

该物品出现在

                                        
                                                                                                    
                    
                                        
                                                                                                    
                    
                                        
                                                                                                    
                    

如何在Catawiki上购买

详细了解我们的买家保障

      1. 发现奇珍异品

      饱览数以千计的专家精选的稀奇物品。查看每件稀奇物品的照片、详情和估价。 

      2. 设置最高出价

      找到您喜欢的物品并设置最高出价。您可以关注拍卖直到最后,也可以让系统为您出价。您只需设置可接受的最高出价。 

      3. 安全支付

      当您付款拍下心仪的稀奇物品后,我们会确保货款的安全,直至物品安然交付与您。我们使用受信赖的支付系统来处理所有交易。 

有类似的东西要出售吗?

无论您是在线拍卖的新手还是专业销售,我们都可以帮助您为您的独特物品赚取更多收入。

出售您的物品