LAKARGIITE Mineral Details

Complete mineralogical data for LAKARGIITE. Chemical Formula: CaZrO3. Crystal System: Orthorhombic. Learn about its geologic occurrence, habit, and identification.

LAKARGIITE

CaZrO3

Crystal System

Orthorhombic

Crystal Class

Dipyramidal

Space Group

Pnma

Point Group

2/m 2/m 2/m

Structure & Data

Crystal Structure

Perovskite-type framework structure is built of interconnected, apex-sharing Zr-octahedra, thus producing distorted channel system occupied by Ca atoms.

Cell Data

a=5.56Å, b=7.93Å, c=5.55Å, Z=”4″

Geology & Identification

Geologic Occurrence

In high-temperature skarns in carbonate-silicate rocks occuring as xenoliths in ignimbrites of volcanic structureLAKARGIITELAKARGIITE

Habit

As submicro pseudocubic crystals

Twinning

90o and 180o about [101], [121]

Relationships

RELATIONSHIP TO OTHER MINERALS

Perovskite group; Zr – analog of perovskite

If you are fascinated by the hidden structures of our planet, you have likely come across LAKARGIITE. 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 LAKARGIITE. 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, LAKARGIITE is defined by the chemical formula CaZrO3.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. LAKARGIITE 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 Dipyramidal.
  • Point Group: 2/m 2/m 2/m
  • Space Group: Pnma
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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 LAKARGIITE, the dimensions of this microscopic building block are:
a=5.56Å, b=7.93Å, c=5.55Å, Z=”4″
The internal arrangement of these atoms is described as:Perovskite-type framework structure is built of interconnected, apex-sharing Zr-octahedra, thus producing distorted channel system occupied by Ca atoms.This 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 LAKARGIITE in the field, what does it actually look like? A mineral’s “habit” describes its typical shape and growth pattern.
  • Common Habit: As submicro pseudocubic crystals
  • Twinning: 90o and 180o about [101], [121]
Twinning is a fascinating phenomenon where two or more crystals grow interlocked in a specific symmetrical pattern. If LAKARGIITE 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.
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Geologic Occurrence: In high-temperature skarns in carbonate-silicate rocks occuring as xenoliths in ignimbrites of volcanic structureKnowing 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. LAKARGIITE is often related to other species, either through similar chemistry or structure.Relationship Data: Perovskite group; Zr – analog of perovskiteUnderstanding 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 LAKARGIITE?The standard chemical formula for LAKARGIITE is CaZrO3. This defines its elemental composition.2. Which crystal system does LAKARGIITE belong to?LAKARGIITE crystallizes in the Orthorhombic system. Its internal symmetry is further classified under the Dipyramidal class.3. How is LAKARGIITE typically found in nature?The “habit” or typical appearance of LAKARGIITE is described as As submicro pseudocubic crystals. This refers to the shape the crystals take when they grow without obstruction.
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4. In what geological environments does LAKARGIITE form?LAKARGIITE is typically found in environments described as: In high-temperature skarns in carbonate-silicate rocks occuring as xenoliths in ignimbrites of volcanic structure. This gives clues to the geological history of the area where it is discovered.5. Are there other minerals related to LAKARGIITE?Yes, it is often associated with or related to other minerals such as: Perovskite group; Zr – analog of perovskite.

External Resources for Further Study

For those looking to dive deeper into the specific mineralogical data of LAKARGIITE, we recommend checking high-authority databases:

Final Thoughts

LAKARGIITE 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 CaZrO3 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.
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