Embryonic Proto-Tethys Ocean: Evidence from the early Ediacaran Kuyake ophiolite mélange along the Altyn Tagh in NW China

Key Points

• Evidence suggests the presence of the proto-Tethys Ocean based on geological formations.
• The early Ediacaran Kuyake ophiolite mélange reveals unique geological characteristics.
• Analysis of the Altyn Tagh range provides critical insights into Earth's tectonic history.
• Understanding this geological context highlights the evolution of oceanic systems.