In this article we are going to explore in depth the topic of Latite, a topic that has been the subject of countless research and debates over the years. Latite is a topic that has captured the attention of people of all ages and backgrounds, and its importance extends to a variety of fields, from science and technology to politics and culture. Through this article, we will seek to shed light on the different aspects of Latite, analyzing its origins, its impact on society and its possible implications for the future. We hope this article serves as an informative and stimulating source for anyone interested in learning more about this fascinating topic.
Volcanic rock | |
Latite is an igneous, volcanic rock, with aphanitic-aphyric to aphyric-porphyritic texture. Its mineral assemblage is usually alkali feldspar and plagioclase in approximately equal amounts. Quartz is less than five percent and is absent in a feldspathoid-bearing latite, and olivine is absent in a quartz-bearing latite. When quartz content is greater than five percent the rock is classified as quartz latite. Biotite, hornblende, pyroxene and scarce olivine or quartz are common accessory minerals. Feldspathoid-bearing latite is sometimes referred to as tristanite.
Rhomb porphyries are an unusual variety with gray-white porphyritic rhomb shaped phenocrysts embedded in a very fine grained red-brown matrix. The composition of rhomb porphyry places it in the trachyte - latite classification of the QAPF diagram.
Latite is found, for example, as lavas in Bulgaria and as intrusive laccoliths and sills in South Dakota, USA.