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Shale with Calcite and Marcasite is a fine-grained, clastic sedimentary rock characterized by its fissility (ability to split into thin layers) and its specific mineralogical composition. The dominant component is shale, composed primarily of clay minerals (e.g., illite, kaolinite, smectite) and fine silt-sized quartz. Interspersed within this matrix are varying amounts of calcite (calcium carbonate) and marcasite (iron disulfide). Calcite may appear as fine grains, shell fragments, fossil remains, or as a cementing agent, often light-colored (white, gray, yellowish). Marcasite typically occurs as brassy yellow to silvery-white, metallic-lustered nodules, concretions, radiating aggregates, or disseminated crystals. The overall color of the shale can range from dark gray to black due to organic matter, or lighter grays, greens, or reds depending on the oxidation state of iron and the presence of other minerals. The presence of marcasite often indicates anoxic depositional conditions.
How to Identify
- Color
- Shale matrix typically dark gray to black (due to organic matter), but can be lighter gray, green, or reddish. Calcite is usually white, gray, or yellowish. Marcasite is brassy yellow to silvery-white, often tarnishing to a dull bronze or iridescent blue/green.
- Luster
- Shale matrix is dull to earthy. Calcite can be vitreous to dull. Marcasite has a metallic luster.
- Texture
- Fine-grained, clastic, fissile (splits into thin layers). Marcasite may form radiating orthorhombic crystals, concretions, or nodules within the fine-grained matrix. Calcite may be microcrystalline, granular, or fossiliferous.
- Crystal Form
- Shale minerals are typically too fine to see individual crystals without magnification. Calcite may show rhombohedral cleavage or be massive/granular. Marcasite forms orthorhombic crystals, often twinned, radiating, or in concretions (e.g., 'cockscomb' marcasite).
- Cleavage
- Shale exhibits fissility (rock cleavage) parallel to bedding. Calcite has perfect rhombohedral cleavage in three directions. Marcasite has indistinct cleavage.
- Geological Environment
- Low-energy, anoxic sedimentary environments such as deep marine basins, stagnant lake bottoms, or swamps, where fine clastic sedimentation, carbonate precipitation, and sulfur-reducing bacteria activity co-occurred.
Key Facts
- Hardness: Shale: 2.5-4 (Mohs). Calcite: 3 (Mohs). Marcasite: 6-6.5 (Mohs).
- Specific Gravity: Shale: 2.0-2.8. Calcite: 2.71. Marcasite: 4.8-4.9.
- Crystal System: Shale: Not applicable (aggregate of fine minerals). Calcite: Trigonal. Marcasite: Orthorhombic.
- Color: Variable for shale (dark gray, black, green, red); white, gray, yellow for calcite; brassy yellow, silvery-white for marcasite.
- Luster: Dull to earthy for shale; vitreous to dull for calcite; metallic for marcasite.
- Transparency: Opaque for shale and marcasite; transparent to translucent for calcite.
- Fracture: Shale: Splintery to conchoidal. Calcite: Conchoidal. Marcasite: Uneven to conchoidal.
- Cleavage: Shale: Fissility (rock cleavage). Calcite: Perfect rhombohedral (3 directions). Marcasite: Indistinct.
- Composition: Shale: Hydrous aluminum silicates (clay minerals), quartz, feldspar. Calcite: Calcium carbonate (CaCO3). Marcasite: Iron disulfide (FeS2).
Quick Check
- Color: Dark gray to black shale matrix; brassy yellow to silvery-white marcasite; white to gray calcite.
- Luster: Dull to earthy for shale; metallic for marcasite; vitreous to dull for calcite.
- Streak: Shale: white, gray, or black (depending on composition). Marcasite: greenish-black to brownish-black. Calcite: white.
Physical Characteristics
- Crystal Habit: Shale: Platy, massive. Calcite: Rhombohedral, granular, massive, fibrous, stalactitic. Marcasite: Orthorhombic, often radiating, tabular, pyramidal, cockscomb aggregates, concretions.
- Cleavage Type: Shale: Fissility (splits along bedding planes). Calcite: Perfect rhombohedral {1011}. Marcasite: Indistinct {101}.
- Fracture Type: Shale: Splintery to conchoidal. Calcite: Conchoidal. Marcasite: Uneven to conchoidal.
- Tenacity: Shale: Brittle. Calcite: Brittle. Marcasite: Brittle.
- Luster Type: Shale: Dull, earthy. Calcite: Vitreous, pearly, dull. Marcasite: Metallic.
Formation
This rock forms in low-energy, anoxic (oxygen-depleted) sedimentary environments, typically marine or lacustrine (lake) settings. Shale, the dominant component, forms from the compaction and lithification of fine-grained clay and silt particles. Calcite precipitates from supersaturated waters, often biogenically (e.g., shell fragments, microfossils) or inorganically, and can occur as cement, nodules, or disseminated grains. Marcasite, an iron disulfide, forms under highly acidic and reducing conditions, often as a diagenetic mineral replacing organic matter or other minerals, or precipitating directly from iron- and sulfur-rich pore waters. The presence of all three indicates a specific depositional and diagenetic history involving fine clastic input, carbonate availability, and anoxic, sulfur-rich conditions.
Usage
While the shale itself can be used as a source for clay in ceramics or cement, or as a low-grade building material, the presence of marcasite and calcite can complicate its industrial use. Marcasite can lead to acid mine drainage if exposed to oxygen and water, and its decomposition can weaken the rock. Calcite can make the shale more susceptible to acid weathering. Historically, some shales with marcasite have been associated with coal seams and have been mined for their sulfur content, though this is less common today. The rock is primarily of scientific interest for understanding paleoenvironments and diagenetic processes.
Age Distribution
Common in sedimentary basins of various ages, from Precambrian to Cenozoic, wherever anoxic conditions and carbonate precipitation occurred alongside clastic deposition.
Where to Find
Illinois Basin, USA
Known for its extensive coal measures and associated shales, which often contain marcasite and calcite, particularly in marine shales overlying coal seams.
Appalachian Basin, USA
Similar to the Illinois Basin, shales associated with coal deposits and marine transgressions can contain these minerals.
North Sea Basin, Europe
Organic-rich shales, such as the Kimmeridge Clay Formation, are known to contain pyrite (polymorph of marcasite) and calcite, indicating similar anoxic conditions.
Western Canada Sedimentary Basin
Various shale formations, particularly those associated with hydrocarbon source rocks, can exhibit these mineral assemblages.
Finding Tips
Look for Dark, Fissile Rocks
Shales are typically dark and split easily into thin layers. The presence of lighter calcite or metallic marcasite will be visible within this matrix.
Check for Metallic Luster
Marcasite's brassy to silvery metallic luster is a key indicator. It often forms distinctive radiating or nodular shapes.
Acid Test for Calcite
A drop of dilute hydrochloric acid (HCl) will effervesce on calcite, indicating its presence. Be cautious with acid and wear appropriate safety gear.
Examine Associated Strata
These shales are often found in association with coal seams, organic-rich layers, or marine fossiliferous beds, indicating the anoxic and carbonate-rich conditions of their formation.
Beware of Weathering
Marcasite is unstable in oxygenated, moist environments and will weather to iron oxides and sulfuric acid. Fresh samples are best found in unweathered outcrops or excavations.
Similar Rocks
Pyritic Shale
Shale with Pyrite (FeS2)
Also known as: Sulfidic Shale
Calcareous Shale
Shale with significant Calcite (CaCO3)
Also known as: Marly Shale
Black Shale
Shale with high organic carbon content
Also known as: Organic-rich Shale
Scientific Classification
- Mineral Class
- Shale: Silicates (clay minerals). Calcite: Carbonates. Marcasite: Sulfides.
- Group
- Shale: Sedimentary rock. Calcite: Calcite group. Marcasite: Pyrite group (polymorph of pyrite).
- Crystal System
- Shale: Not applicable (rock). Calcite: Trigonal. Marcasite: Orthorhombic.
- Chemical Formula
- Shale: Variable (e.g., Al2Si2O5(OH)4 for kaolinite). Calcite: CaCO3. Marcasite: FeS2.
- Composition
- Shale: Predominantly clay minerals, quartz, feldspar, micas. Calcite: Calcium carbonate. Marcasite: Iron disulfide (46.55% Fe, 53.45% S).
Explore Shale with Calcite and Marcasite
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