Potash Feldspar Lumps

Potash Feldspar Lumps are important minerals which is mostly use in a wide variety of industries like ceramics as a raw material. Also, this mineral product is available in a huge and bulk amount by the THREETA international trading group from the origin of Iran. Also, this country is one of the main resources for extracting valuable minerals. Mostly in the desert belt area, the potash feldspar lumps are extracting. The most competitive advantage of this product is the affordability of this mineral component to supply from Iran. Are you an activist in the field for supplying raw mineral products? For the attention of factory owners for aggregates, glass, and ceramics. Please do not hesitate to have a look at the Iranian potash feldspar lumps. However, our experts 24/7 on your service to answer your queries about this material.

A Brief  About the Potash Feldspar (Potassium Feldspars) Lumps:

Potassium feldspars is an important component among igneous rocks. Their crystal shape particularly is developing in pegmatites. The crystalline igneous rocks that form during late water-wet stages of magma cooling. Within the potash feldspar lumps group, the occurrence of each potassium feldspar member varies slightly. Orthoclase is the most common potassium feldspar, forming the majority of potassium feldspar in igneous rocks.

This mineral generally is using as decorative targets for making a artificial stone to create eyecatching accessories which could bring the beauty and prettiness in your atmpsphere. The presented potash feldspar lumps has enough ordered crystal structure than orthoclase and is primarily found in volcanic igneous rocks. Where magmas cooled more rapidly and crystals had less time to form. Microcline tends to form at lower temperatures and is the most common found in pegmatites, low-temperature hydrothermal veins, and some low-grade metamorphic rocks. It may also occur in significant amounts in granite.