I. Official Name: Seymchan
Type: Pallasite (PMG-an, Main Group anomalous)
Discovery Date: June 1967
Discovery Location: Riverbed of the Hekandue River (tributary of the Yasachnaya River), Magadan Oblast, Russia
Coordinates: 62°54′ N, 152°25′ E
Discoverers: F. A. Mednikov (main mass), I. H. Markov (secondary mass)
II. Discovery History
1. June 1967: Geologist Mednikov discovered the 300 kg main mass.
2. October 1967: Markov found a 51 kg secondary mass 20 meters away.
3. Initial Classification: Samples taken only from the metal portion; mistakenly classified as a IIE iron meteorite.
4. 2004: An expedition discovered approximately 50 kg of new fragments; 20% of these contained olivine.
5. 2007: Officially reclassified as a Main Group pallasite (PMG-an).
6. Largest Fragment: Approximately 1.5 tons; currently housed at the Moscow Planetarium.
III. Minerals and Composition
- Matrix: Iron-nickel alloy (nickel content approx. 9.15%)
- Olivine: Translucent to transparent; emerald green to yellowish-brown; large, centimeter-scale crystals
- Accessory Minerals: Troilite, chromite, schreibersite, apatite, etc.
- Characteristics: High iridium (Ir) content → Classified as "anomalous" (an)
- Structure: Biphasic/Heterogeneous – Pure iron-nickel zones (showing Widmanstätten patterns)
- Olivine-rich zones (olivine embedded in metal)
IV. Seymchan Meteorite: Complete Elemental Analysis Table
Metal Phase (Iron-Nickel Matrix) Major Elements (Weight Percentage wt%)
Mineral Phase | Fe | Ni | Co | P | Total
Kamacite (Kamacite, α-Fe) 92.16% 6.59% 0.50% 0.02% 99.26%
Taenite (γ-Fe) 43.7% 54.4% 0.2–0.55% 0.20% –
Schreibersite 45.17% 39.9% 0.13% 14.8% 100%
V. Metal phase: Trace elements (INAA - Instrumental Neutron Activation Analysis, ppm / μg/g)
Element Content (ppm) Element Content (ppm)
Nickel (Ni) 92,800–95,100 (9.28–9.51%) Gallium (Ga) 24.6–26.3
Cobalt (Co) 5,260–5,330 (0.53%) Germanium (Ge) 68.3
Chromium (Cr) 13–31 Arsenic (As) 18.2–18.8
Copper (Cu) 121–152 Tungsten (W) 0.34–0.52
Iridium (Ir) 0.66–0.69 Gold (Au) 2.01–2.13
VI. Olivine phase (Olivine, Fa₁₁.₆) composition
- Average formula: (Mg₁.₇₅₁Fe₀.₂₃₀Mn₀.₀₀₆)SiO₄
- Magnesium (MgO): 49–50%
- Iron (FeO): 11–12%
- Silicon (SiO₂): 38–39%
- Manganese (MnO): 0.2%
- Nickel (Ni): <110 ppm (very low)
VII. Other accessory minerals (trace amounts)
- Troilite (FeS): Fe 59.38%, S 38.11%, Ni 0.08%
- Chromite: Cr 35.45%, Fe 15.24%, Mg 43.71%
VIII. Key Characteristics
- High nickel (9.15–9.5%) and high iridium (~0.68 ppm) → Classified as PMG-an (Main Group anomalous pallasite)
- Low phosphorus and sulfur content, minimal impurities → Highly stable, resistant to rusting
- Dual-phase structure: Pure iron-nickel zones (displaying Widmanstätten patterns) + olivine-rich zones.