Today, Latite is a topic of great relevance and interest to a wide audience. With the advancement of technology and globalization, Latite has taken a leading role in today's society, generating multiple debates, discussions and developments in different areas. From academia and science to business and politics, Latite has captured the attention of experts and fans alike. In this article, we will explore the different facets and dimensions of Latite, analyzing its impact and relevance in the current context. Without a doubt, Latite is a topic that deserves to be delved into and discussed in depth.
Volcanic rock | |
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Latite is an igneous, volcanic rock, with aphanitic-aphyric to aphyric-porphyritic texture. It is the volcanic equivalent of monzonite. 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.[1] Biotite, hornblende, pyroxene and scarce olivine or quartz are common accessory minerals. Feldspathoid-bearing latite is sometimes referred to as tristanite.[2]
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[3] and as intrusive laccoliths and sills in South Dakota, USA.[4]