The Carolina Terrane, also called the Carolina Superterrane or Carolinia, is an exotic terrane running ~ approximately North-South from central Georgia to central Virginia in the United States. It constitutes a major part of the eastern Piedmont Province. The terrane likely formed as a subduction-related volcanic island arc off the coast of South America during the Neoproterozoic to Early Cambrian. Plate tectonics moved it across the Iapetus Ocean until it docked with Laurentia. The date of the docking is unknown, but could have occurred during the Taconic, Acadian, or Alleghanian Orogenies. The terrane comprises Neoproterozoic to Early Cambrian meta-sedimentary and meta-igneous rocks, intruded by later Paleozoic plutons. The protoliths of the meta-igneous rocks include mafic, intermediate, and felsic volcanics and plutons. These rocks underwent at least four metamorphic/deformation events, and so their original textures and mineralogies have been significantly altered. As with related peri-Gondwanan terranes, the Carolina Terrane played a major role in the tectonic evolution of the east coast of North America during the Paleozoic. It represents the largest exotic terrane in the Appalachians, and underlies an enormous area of the southeastern United States.
Origin and Evolution
The Carolina Terrane's history begins in the Neoproterozoic, as the Rodinia supercontinent was breaking apart:
Island Arc Formation. Between 625 and 550 Ma, a subduction zone initiated in the Paleoasian Ocean between Baltica and Gondwana. The subduction produced a string of volcanic island arcs off the coast of Gondwana, including the Carolina Terrane, Avalonia microcontinent, and Gander Terrane. It is unclear whether the arc formed on oceanic or continental crust.
Opening of the Iapetus Ocean. As the Rodinia supercontinent continued to break apart, the Iapetus Ocean opened, splitting apart Laurentia, Baltica and Gondwana. The opening may have started as early as 760 Ma, though the major part appears to be later, and the southern portion may not have finish until 550 Ma.
Metamorphic/Deformation Event of Unknown Cause: Upper-crustal folding, faulting, and mineral foliation during the Late Neoproterozoic / Early Cambrian ; it is unclear whether this represents a regional or local event, or event what the event was. Proposed possible causes include back-arc rifting or closure, subduction of another block, or collision of the Charlotte and Carolina terranes.
Migration of the Island Arcs & Opening of the Rheic Ocean. At some point in the Late-Cambrian/Early-Ordovician, the subduction zone off the coast of Gondwana caused a back-arc basin to rift. The new spreading center opened the Rheic Ocean between the Carolina-Avalonia-Gander terranes and Gondwana. The combination of slab rollback and ridge-push moved the Carolina-Avalonia-Gander terranes north across the Iapetus Ocean, toward Laurentia and Baltica. Avalonia would dock with Baltica before they both collided with Laurentia; the Carolina Terrane appears to have not docked with Baltica.
Metamorphic/Deformation Event of Unknown Cause: The Carolina Terrane underwent another metamorphic event during the Late Ordovician/Silurian, which brought its rocks to greenschist facies. This time period broadly conforms to the Taconic Orogeny, and could represent the docking of Carolina onto Laurentia.
Cat Square Terrane Formation. As the Carolina Terrane approached Laurentia, the Cat Square Terrane formed in the ocean basin between Laurentia and the approaching Carolina Terrane. It's possible it formed as an accretionary prism in front of the Carolina Terrane.
Metamorphic/Deformation Event of Unknown Cause: The Carolina Terrane underwent another metamorphic event during the Devonian. This time period broadly conforms to the Acadian Orogeny, and could represent the docking of Carolina onto Laurentia.
Docking with Laurentia. It is unclear exactly when the Carolina Terrane docked with Laurentia. Hypotheses include accretion during the Taconic Orogeny, Acadian Orogeny, or Alleghanian Orogeny. See summary of evidence for each in.
Alleghanian Metamorphism. The Carolina Terrane was metamorphosed again during the Alleghanian Orogeny, reaching greenschist facies in the Eastern Slate Belt and amphibolite facies in the Charlotte Terrane.
Relationships to Nearby Terranes
The Carolina Terrane is part of the larger Carolina Zone, which includes several related terranes: the Charlotte Terrane, Falls Lake Terrane, Crab Tree Terrane, Raleigh Terrane, Spring Hope Terrane, Roanoke Rapids Terrane, Uchee Terrane, Savannah River Terrane, Augusta Terrane, Milledgeville Terrane, Triplet Terrane, and Dreher Shoals Terrane. In addition to the related terranes of the Carolina Zone, the Carolina Terrane is adjacent to several possibly-unrelated terranes, including:
Cat Square Terrane. a strip of metamorphosed sedimentary rocks east of the Tugaloo Terrane. These rocks were likely deposited as greywackes and pelites between 430 and ~380 million years ago. They were likely originally deposited in the shallow ocean basin between Laurentia and the approaching Carolina Terrane.
Goochland Terrane: a strip of metamorphic rocks running along the northeast boundary of the Carolina Terrane. It is unclear how this zone is related to the Carolina Terrane. The Raleigh-Goochland Terrane is intruded by Neoproterozoic alkalic granite plutons, which could be related to Carolina Terrane arc volcanism, or the plutons could be related to Rodinia-related rifting along the margins of Laurentia.
