A new state of matter; the 5th state of matter: a new type of metamorphic origin superionic metablastic solids/rocks/minerals
Authors: Tarhan Niyazi 
Published: August 2024

Leucocratoblastic metablastic rock series and their derivatives (known as granite/granitoid, gabbro/gabbroid, diorite/dioritoid, charnockite/charnockite and carbonatite/carbonatoid intrusions, plutons and batholiths of magmatic origin), which are a type of new modern metamorphic rocks, developed within the regional dynamothermal Tarhan metamorphism cycle, and are in the Abukuma type reversed regional regressive dynamothermal metamorphism type/stage where temperatures are effective compared to pressures (T>P, temperatures mark the metamorphism); The pre-exiting primary source rock units (cosmic upper mantle peridotites, continental magmatic rock sequence/ocean crust sequence/ophiolite series, ensialic-ensimatic island arc origin volcanosedimentary series, volcanic and different sedimentary rock units etc.) formed at different ages, origins and environments and the classical metamorphic equivalent of Barrow type regional progressive dynamo-thermal metamorphism where the pressures are effective compared to the temperatures of the primary source rock units (P>T, pressures mark the metamorphism) within different metamorphic rocks (micacite, amphibolite, marble etc.) are derived from them in solid phase and in-situ (autochthonous where they exist). Modern leucocratoblastic metablastic rock series and derivatives of metamorphic origin; They correspond to modern metamorphic rocks that are different in physical properties (texture, structure, color, mineralogical composition) from the known classical metamorphic rocks (mica schist, amphibolite, marble, etc.) of the known classical regional progressive dynamo-thermal metamorphism (also known as the single type, single component, unidirectional regional metamorphism that forms metamorphic belts) of the previously existing (pre-exiting) primary source rocks from which they were derived in solid phase and in-situ; but have the same chemical composition, are allotropic and a kind of new generation (3rd generation metamorphic source material/rock/minerals, etc.). In other words; modern leucocratoblastic metablastic rock series and their derivatives of metamorphic origin have developed as a result of the allotropic phase change of previously existing (pre-exiting) solid matter/rock/minerals in the regional dynamothermal Tarhan metamorphism cycle into another new generation (3rd generation) solid matter/rock/minerals with different physical properties in the solid phase and in-situ but the same chemical composition. This phase change, which occurs with the change and transformation of solid matter/rock/minerals in the solid phase and in-situ to allotropic new matter/rock/minerals in another solid phase, was first defined and named as superionic metablastic solid matter/rock/minerals. For this reason; granite mineralogical composition enriched and dominant superionic metablastic solid leucocratoblastic metablastic rock series and derivatives and superionic metablastic solid rock forming felsicoblast crystalloblast neominerals correspond to the 5th state of matter. Superionic metablastic solid matter/metablastic rock/crystalloblast neominerals corresponding to the 5th state of the mineral have developed spontaneously in the natural environment and under natural conditions. They have not developed under any external influence, coercion, intervention or extraordinary conditions (artificial means in a laboratory environment). They have been included in the classical states of matter (solid, liquid, gas, plasma) that can be seen in our daily lives as the 5th state of matter. Or, they should be accepted and proposed as a separate, new modern 5th state of matter.