（Temporarily Out of Stock — Contact Us for Availability）Seymchan Pallasite Meteorite Specimen, Half-Cut Russian Meteorite with Olivine Crystals, 2546g Natural Space Rock

（Temporarily Out of Stock — Contact Us for Availability）Seymchan Pallasite Meteorite Specimen, Half-Cut Russian Meteorite with Olivine Crystals, 2546g Natural Space Rock

Name: （Temporarily Out of Stock — Contact Us for Availability）Seymchan Pallasite Meteorite Specimen, Half-Cut Russian Meteorite with Olivine Crystals, 2546g Natural Space Rock
Brand: Fancying Secret
Availability: OutOfStock

$0.00

Color

بني Silver

كمية

This is a one-of-a-kind Seymchan pallasite meteorite specimen from Russia, featuring a dramatic half-cut surface with natural olivine crystals embedded within an iron-nickel matrix. The polished cross-section reveals a rare contrast of metallic structure, translucent yellow-green olivine, and natural outer crust, making it both a scientific specimen and a striking display piece.

Officially known as the Seymchan meteorite, this material was first discovered in 1967 in the Magadan Region of Russia. Seymchan was later reclassified as a rare pallasite meteorite, a type believed to originate from the boundary between an asteroid’s metallic core and rocky mantle. Its structure combines iron-nickel metal with olivine crystals, creating a natural record of ancient planetary formation.

The specimen weighs approximately 2546g and measures about 163 × 83 × 69 mm. Its iron-nickel body contains visible Widmanstätten patterns in metallic areas, while the olivine-rich zones show green to golden-brown crystal inclusions. The 1 cm reference cube shown in the photos is used for scale.

With its substantial size, natural texture, and rare cosmic origin, this Seymchan meteorite is ideal for collectors, museum-style displays, office décor, astronomy enthusiasts, and meaningful luxury gifting. Each piece is photographed individually, and the item you see is the exact specimen you will receive.

Lifetime authenticity guarantee. This is a genuine natural meteorite specimen, not artificial stone, replica, or ordinary mineral.

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.

عزيزتي:

فانسينغ سيكريت - حيث ترتدين الكون.
فانسينغ سيكريت - حيث ترتدين الكون. ليس بالضرورة أن تشعري بثقل كل ما تحملينه. في معظم الأيام، ليس العالم هو ما يرهقكِ، بل الضجيج المستمر في رأسكِ، والضغط المستمر لفهم كل شيء، لتكوني أفضل، أسرع، أقوى،
ولكي لا تتخلفي عن الركب.

لكن انظري إلى الوراء قليلاً، وستجدين أن شيئًا ما يتغير. ما يبدو ضخمًا الآن يصبح لحظة عابرة. لأن الحقيقة هي:

أنتِ تعيشين داخل شيء أعظم بكثير من أي قلق.

هذه القطع التي ترتدينها لم تُصنع على الأرض.

لقد سافرت عبر الفضاء لأكثر من 4.6 مليار سنة - عبر الصمت، والاصطدام، والدمار، والولادة من جديد - قبل أن تصل إلى هنا.

إنها لا تحمل مجرد مواد،

إنها تحمل الزمن.

في فانسينغ سيكريت،

لا نحول النيازك إلى مجوهرات فحسب. نُحوّل ما كان خامًا، جامحًا، وبعيد المنال إلى شيءٍ يمكنكِ ارتداؤه بالفعل - شيءٌ تشعرين فيه بالقرب، والقصد، والجمال الإنساني. كل شيء في الكون مُعدٌّ للارتداء، لأن

لكن هذا الشيء كذلك.

لسنا هنا لنقدم لكِ إجابات.

نحن هنا لنذكركِ بمنظورٍ مختلف.

أنه ليس عليكِ معرفة كل شيء.

أنه من حقكِ أن تشعري بالضآلة أحيانًا.

وأن الضآلة لا تعني عدم الأهمية.

عندما ترتدينه،

تتذكرين:

أنتِ لستِ وحدكِ في هذه اللحظة.

أنتِ جزءٌ من شيءٍ عظيم.

وبطريقةٍ ما،

لا تزالين كافية.

فانسيينغ سيكريت