

Petrographic Polarizing Microscope
岩相偏光显微镜
- SKU POM-0001
- Polarizing Microscopes
- CE (to be confirmed)
- ISO 9001 manufacturing (to be confirmed)
Price on request — FOB / CIF quoted per order
Prices depend on configuration, quantity and destination port.
Key specifications
| Optical system | Infinite corrected, strain-free |
|---|---|
| Magnification range | 40×–600× |
| Objectives | 4×, 10×, 40×, 60× strain-free |
| Stage | Rotating 360°, graduated 1° |
| Polarizers | Polarizer and analyser, crossed |
| Bertrand lens | Focusable, centrable |
By Lab Manufacturers China Technical TeamLast reviewed Standards: ISO 8036, ISO 19012-1, ASTM E3
What is the Petrographic Polarizing Microscope?
A petrographic polarizing microscope is designed for transmitted-light study of thin sections of rocks and minerals. It combines crossed polarizers, a rotating centred stage and conoscopic observation for identification in geology laboratories.
What is the Petrographic Polarizing Microscope?
A petrographic polarizing microscope is designed for transmitted-light study of thin sections of rocks and minerals. It combines crossed polarizers, a rotating centred stage and conoscopic observation for identification in geology laboratories.
Overview
A petrographic polarizing microscope uses transmitted polarized light to examine thin sections of rocks and minerals mounted on glass slides. A polarizer below the stage and an analyser above can be crossed, and a rotating, centred stage with a graduated scale allows extinction angles to be measured. A Bertrand lens and accessory plates, such as a quarter-wave or full-wave plate, support conoscopic observation and retardation estimates. Strain-free objectives prevent the optics from adding false birefringence. The instrument identifies minerals from their refractive indices, interference colours, extinction behaviour and interference figures, and is a core tool of geology and mineralogy.
How does it work?
A polarizing microscope places a polarizer below the specimen and an analyser above it, usually with their transmission directions crossed. Isotropic materials appear dark under crossed polarizers, while anisotropic materials split light into two rays and change its polarization, producing interference colours and extinction positions as the stage rotates. With a full-wave plate and accessory plates, retardation and optical sign can be estimated, and conoscopic observation with a Bertrand lens shows interference figures that identify crystal systems and optic axes. A rotating, centred stage with graduated scale allows precise angle measurement. Polarized light therefore converts differences in crystal orientation and refractive index into visible colours and extinction behaviour.
What are the key features?
- Transmitted polarized light with crossed polarizers
- Rotating centred stage with graduated scale
- Bertrand lens for conoscopic observation
- Accessory plates for retardation estimates
- Strain-free objectives for accurate polarimetry
What are the technical specifications?
A typical petrographic polarizing microscope configuration offers optical system of Infinite corrected, strain-free, magnification range of 40×–600×, objectives of 4×, 10×, 40×, 60× strain-free, stage of Rotating 360°, graduated 1°, polarizers of Polarizer and analyser, crossed and bertrand lens of Focusable, centrable. Values are indicative of the product class; the exact figures for each configuration are confirmed on the quotation and the calibration documents supplied with the instrument.
Which applications is it used for?
The Petrographic Polarizing Microscope is used in geological thin-section analysis, mineral identification, ceramic and cement clinker study and teaching of optical mineralogy. Across the wider Polarizing Microscopes class, laboratories also deploy it for mineral and rock identification, crystal and pharmaceutical polymorph study and fibre and polymer orientation analysis.
Which standards and certifications apply?
Relevant standards and methods include ISO 8036, ISO 19012-1, ASTM E3, ISO 7404-3 and IEC 61010-1. Certification candidates for this model are CE and ISO 9001 manufacturing; each is to be confirmed for the specific configuration before shipment, and certificates are supplied only where they have been issued.
Centre and focus the rotating stage so the specimen stays in view, and calibrate the crosshair and scale against a known reference before measuring angles. Use strain-free objectives and keep polarizer and analyser clean; strain in optics or contamination produces false colours and extinction. Set the analyser accurately to extinction with no specimen in place. For quantitative retardation work, verify accessory plates and compensators and record their orientation. Avoid heat and vibration, which disturb optical alignment, and store the microscope with accessories protected. Recalibrate after service.
How do I select the right Petrographic Polarizing Microscope?
Choose a petrographic polarizing microscope for transmitted-light study of thin sections and crystals. Confirm the stage rotates and is centred with a graduated scale, that strain-free objectives and a Bertrand lens are available, and that accessory plates for retardation work are supplied. For quantitative identification, verify the calibration of the scale and the quality of the polarizers.
How does it compare with other Polarizing Microscopes variants?
Choose a polarizing microscope when optical anisotropy must be studied, such as identifying minerals, crystals, fibres or polymer structure. Decide whether transmitted polarized light is sufficient or whether reflected polarized light is also needed for opaque ores and polished sections. Confirm the stage rotates and is centred, and that a graduated scale with vernier is present for angle measurement. Consider whether strain-free objectives, a Bertrand lens, accessory plates and a conoscopic path are required. For quantitative work, a compensator and calibrated plates may be needed. Digital models add imaging and measurement software.
Full specifications
| Optical system | Infinite corrected, strain-free |
|---|---|
| Magnification range | 40×–600× |
| Objectives | 4×, 10×, 40×, 60× strain-free |
| Stage | Rotating 360°, graduated 1° |
| Polarizers | Polarizer and analyser, crossed |
| Bertrand lens | Focusable, centrable |
| Accessory plates | Quarter-wave and full-wave |
| Eyepiece | 10× with crosshair |
| Illumination | Transmitted, LED or halogen |
| Power supply | 100–240 V AC |
Indicative values for this product class. Final specifications are confirmed on the quotation and in the calibration documents supplied with the instrument.
Applications
- Geological thin-section analysis
- Mineral identification
- Ceramic and cement clinker study
- Teaching of optical mineralogy
Key features
- Transmitted polarized light with crossed polarizers
- Rotating centred stage with graduated scale
- Bertrand lens for conoscopic observation
- Accessory plates for retardation estimates
- Strain-free objectives for accurate polarimetry
Frequently asked questions about Petrographic Polarizing Microscope
Minerals can be identified from refractive index, birefringence and interference colours, extinction angle, pleochroism and interference figures. Rocks are classified from the mineral assemblage and textures seen in thin section. The method is standard in geology and mineralogy.
A centring objective or centring screws bring the rotation axis of the stage into coincidence with the optical axis of the microscope. This ensures a feature stays in the field and does not wander as the stage rotates, which is essential for accurate extinction-angle measurement.
Accessory plates add a known retardation to the specimen, shifting interference colours so that the order and sign of birefringence can be determined. A quarter-wave plate helps distinguish fast and slow directions, and a full-wave plate makes subtle colour changes easier to see.
Birefringence is the property of anisotropic materials to split a light ray into two rays that travel at different speeds and have different refractive indices. Under crossed polarizers it produces interference colours and characteristic extinction as the specimen rotates, which helps identify and study such materials.
Rotating the stage changes the orientation of the specimen relative to the polarizers, so the extinction positions and interference colours can be observed and measured. The graduated scale and vernier let the extinction angle be read and compared with reference data for identification.
Orthoscopic observation uses parallel light to form a normal image of the specimen, showing interference colours and extinction. Conoscopic observation inserts a Bertrand lens to converge the light and form an interference figure in the back focal plane, revealing optic axes and helping determine the crystal system.
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