Ophiolittisis

Ophiolittisis is a term that has been used informally and inconsistently in scientific literature, primarily in relation to the geological phenomenon of ophiolite emplacement and the associated geological processes. It is not a formally recognized geological term or a defined scientific concept. The term appears to stem from the combination of "ophiolite," which refers to a section of oceanic crust and upper mantle that has been uplifted and exposed on land, and "-isis," a suffix often denoting a condition or state.

When the term has appeared, it has sometimes been used to describe the complex geological conditions and processes involved in the obduction of ophiolite sequences. This can include the deformation, metamorphism, and fracturing that occur as these oceanic fragments are thrust onto continental crust. It may also allude to the unique mineral assemblages and rock types found within ophiolites, which reflect their origin in the deep ocean and the subsequent geological events they have undergone. Due to its informal and varied usage, understanding the specific meaning of "ophiolittisis" requires careful attention to the context in which it is employed within a given publication. It is generally advisable to use more precise and established geological terminology when discussing ophiolite-related phenomena.