Microcontinents and Continental Fragments Associated With Subduction Systems

• Published in: Tectonics (Washington, D.C.) Vol. 39; no. 8
• Main Authors: Broek, J. M., Gaina, C.
• Format: Journal Article
• Language: English
• Published: 01.08.2020
• Subjects: continental crust evolution; continental fragments; continental rifting; microcontinents; subduction; subduction dynamics
• ISSN: 0278-7407; 1944-9194
• DOI: 10.1029/2020TC006063

Microcontinents and continental fragments are small pieces of continental crust that are surrounded by oceanic lithosphere. Although classically associated with passive margin formation, here we present several preserved microcontinents and continental fragments associated with subduction systems. They are located in the Coral Sea, South China Sea, central Mediterranean and Scotia Sea regions, and a “proto‐microcontinent,” in the Gulf of California. Reviewing the tectonic history of each region and interpreting a variety of geophysical data allows us to identify parameters controlling the formation of microcontinents and continental fragments in subduction settings. All these tectonic blocks experienced long, complex tectonic histories with an important role for developing inherited structures. They tend to form in back‐arc locations and separate from their parent continent by oblique or rotational kinematics. The separated continental pieces and associated marginal basins are generally small and their formation is quick (<50 Myr). Microcontinents and continental fragments formed close to large continental masses tend to form faster than those created in systems bordered by large oceanic plates. A common triggering mechanism for their formation is difficult to identify, but seems to be linked with rapid changes of complex subduction dynamics. The young ages of all contemporary pieces found in situ suggest that microcontinents and continental fragments in these settings are short lived. Although presently the amount of in‐situ subduction‐related microcontinents is meager (an area of 0.56% and 0.28% of global, non‐cratonic, continental crustal area and crustal volume, respectively), through time microcontinents contributed to terrane amalgamation and larger continent formation. Key Points Microcontinents can form in association with convergent plate boundaries which experienced long and complex histories Formation often requires oblique or rotational kinematics as well as the presence of inherited structures in the continental crust Changes in slab dynamics is a potential mechanism that drives microcontinent formation in convergent settings