If you are fascinated by the hidden structures of our planet, you have likely come across
GODLEVSKITE. This mineral is a compelling subject for study, offering a unique glimpse into the complex chemistry that shapes the Earth’s crust.Whether you are a student identifying a hand sample, a researcher looking for crystallographic data, or a collector curious about a new find, this guide breaks down everything you need to know about
GODLEVSKITE. From its precise chemical formula to the geological environments where it thrives, let’s explore what makes this mineral distinct.
The Chemistry Behind the Crystal
Every mineral tells a story through its chemistry. At its core,
GODLEVSKITE is defined by the chemical formula
(Ni,Fe)9S8.This isn’t just a string of letters and numbers; it represents the precise recipe of elements that nature used to build this specimen. This specific chemical composition is what gives the mineral its stability and dictates how it reacts with acids, heat, or other minerals. It is the fundamental “DNA” that geologists use to classify it within the larger mineral kingdom.
Crystallography: Geometry in Nature
One of the most beautiful aspects of mineralogy is the hidden geometry within every stone.
GODLEVSKITE crystallizes in the
Orthorhombic system.Think of this as the mineral’s architectural blueprint. It dictates the symmetry and the angles at which the crystal faces grow. Digging deeper into its symmetry, it falls under the
Disphenoidal.
- Point Group: 2 2 2
- Space Group: C222
Why does this matter? These crystallographic details are like a fingerprint. They influence optical properties—how light travels through the crystal—and physical traits like how it breaks or cleaves when struck.
Internal Structure and Unit Cell
If we could zoom in to the atomic level, we would see the “Unit Cell”—the smallest repeating box of atoms that builds up the entire crystal. For
GODLEVSKITE, the dimensions of this microscopic building block are:
a=9.18Å, b=11.26Å, c=9.46Å, Z=4
The internal arrangement of these atoms is described as:
Compounds of metals with S, Se, Te (chalcogens) & As, Sb, Bi (metalloids); metal sulfides, M:X > 1:1; edge-sharing Ni[S4] tetrahedra from 3-membered chains // [100], [001], [001], [010] chains form 5-membered cross; edge-sharing Ni[S5] □∆ form [4]- clusters & chains // [101].1 Unusual having CN = 4, while S has CN = 6, which leads to unusual formula characterisic of anti-structures.2 Based on distorted cubic close-packed array of 32 S atoms per unit cell with 20 Ni atoms in tetrahedral coordination & 16 in □∆ coordination; ideal stoichiometry is established as Ni9S8; NiS4 tetrahedra form clusters of 3-membered chain & 5-membered crosses, & NiS5 □∆ form [4]-clusters & chains; structure contains elements of structures of related phases α-Ni7S6, millerite (NiS) & pentlandite [(Fe,Ni)9S8].3 Structure of godlevskite & synthetic Ni9S8 is hybrid of structural elements of pentlandite, millerite & α-Ni7S6; unlike millerite, α-Ni7S6 & heazlewoodite, structure does not contain [3]-clusters (Ni3) of short Ni—Ni distances.4This internal structure is the invisible framework that supports everything we see on the outside, from the mineral’s density to its hardness.
Physical Appearance (Habit)
When you find
GODLEVSKITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
- Common Habit: As aggregates and single micro grains; as fine disseminations
- Twinning: Perpendicular to (101), sometimes in geniculated forms
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If GODLEVSKITE exhibits twinning, it can be a dead giveaway for identification, distinguishing it from look-alike minerals.
Where is it Found? (Geologic Occurrence)
Minerals are the products of their environment. They don’t just appear anywhere; they need specific conditions—pressure, temperature, and chemical ingredients—to form.
Geologic Occurrence:
In hydrothermal veins; in peridotite with other nickel sulfidesKnowing this context helps geologists reconstruct the history of a rock formation. It tells us whether the rock was born from cooling magma, settled in an ancient ocean, or was transformed by the intense heat and pressure of metamorphism. For more broad geological context, resources like the
U.S. Geological Survey (USGS) provide excellent maps and data.
Related Minerals
No mineral exists in a vacuum.
GODLEVSKITE is often related to other species, either through similar chemistry or structure.
Relationship Data:
Compare pentlanditeUnderstanding these relationships is key. It helps us see the “family tree” of the mineral world, showing how different elements can substitute for one another to create an entirely new species with similar properties.
Frequently Asked Questions (FAQs)
1. What is the chemical formula of GODLEVSKITE?The standard chemical formula for GODLEVSKITE is
(Ni,Fe)9S8. This defines its elemental composition.
2. Which crystal system does GODLEVSKITE belong to?GODLEVSKITE crystallizes in the
Orthorhombic system. Its internal symmetry is further classified under the Disphenoidal class.
3. How is GODLEVSKITE typically found in nature?The “habit” or typical appearance of GODLEVSKITE is described as
As aggregates and single micro grains; as fine disseminations. This refers to the shape the crystals take when they grow without obstruction.
4. In what geological environments does GODLEVSKITE form?GODLEVSKITE is typically found in environments described as:
In hydrothermal veins; in peridotite with other nickel sulfides. This gives clues to the geological history of the area where it is discovered.
5. Are there other minerals related to GODLEVSKITE?Yes, it is often associated with or related to other minerals such as:
Compare pentlandite.
External Resources for Further Study
For those looking to dive deeper into the specific mineralogical data of
GODLEVSKITE, we recommend checking high-authority databases:
Final Thoughts
GODLEVSKITE is more than just a name on a list; it is a testament to the orderly and beautiful laws of nature. With a chemical backbone of
(Ni,Fe)9S8 and a structure defined by the
Orthorhombic system, it holds a specific and important place in the study of mineralogy.We hope this overview has helped clarify the essential data points for this specimen. Whether for academic study or personal interest, understanding these properties brings us one step closer to understanding the Earth itself.
