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Macro & Micro-Core 3rd Axes ConversionMacro & Micro-Core 3rd Axes Conversion
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Macro & Micro-Core 3rd Axes Conversion

$10,429.00

Actual product specifics may vary depending upon the needs of the customer.  This is a 3rd axes implementation allowing for large panoramic imaging and focus stacking using 3 axes of automation.  Iterations are specifically designed for clients seeking high resolution imagery of soil boxes, insect boxes, core boxes, tree core boxes or any other object having a significant length x width.

 

The complete playlist can be viewed on our YouTube Channel here: https://www.youtube.com/watch?v=Whoa4jDUYo8&list=PLcKIGvtblfut6S-o7jE01siFfMwwFHQsO

 

White Marble before HCl
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Gneiss from Queenstown, New Zealand

$19.00 – $400.00

Gneiss ( /ˈnaɪs/) is a common distributed type of rock formed by high-grade regional metamorphic processes from pre-existing formations that were originally either igneous or sedimentary rocks. It is often foliated (composed of layers of sheet-like planar structures). The foliations are characterized by alternating darker and lighter colored bands, called “gneissic banding”.

White Marble before HCl
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Polished K Feldspar-Epidote-Quartz-Biotite Matrix

$19.00 – $400.00

Feldspars are a group of rock-forming tectosilicateminerals that make up about 41% of the Earth‘s continental crust by weight.[2]

Feldspars crystallize from magma as veins in both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock.[3] Rock formed almost entirely of calcic plagioclase feldspar (see below) is known as anorthosite.[4] Feldspars are also found in many types of sedimentary rocks.[5]

White Marble before HCl
Select options This product has multiple variants. The options may be chosen on the product page

Polished K Feldspar-Epidote-Quartz-Biotite Matrix

$19.00 – $400.00

Feldspars are a group of rock-forming tectosilicateminerals that make up about 41% of the Earth‘s continental crust by weight.[2]

Feldspars crystallize from magma as veins in both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock.[3] Rock formed almost entirely of calcic plagioclase feldspar (see below) is known as anorthosite.[4] Feldspars are also found in many types of sedimentary rocks.[5]