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The Panama microplate is bordered to the north by the Panama deformed belt and a diffuse thrust belt in the Cordillera Central of Costa Rica. These thrust belts are being controlled by the active convergence of the Caribbean plate towards Central America.
The Panama fracture zone is a major, active right lateral-moving transform fault and associated inactive fracture zone which forms part of the tectonic boundary between the Cocos plate and the Nazca plate, the Cocos–Nazca spreading centre.
The geology of Costa Rica is part of the Panama Microplate, which is slowly moving north relative to the stable Caribbean Plate. [1] [2]In the late Cretaceous, an oceanic trench or backarc system formed in connection with a subduction zone, situated where the Isthmus of Panama is now located.
Sangihe plate – Microplate within eastern Indonesia; Okinawa plate – Minor tectonic plate from the northern end of Taiwan to the southern tip of Kyūshū; Pelso plate – Small tectonic unit in the Pannonian Basin in Europe; Timor plate – Microplate in Southeast Asia carrying the island of Timor and surrounding islands
The Coiba plate is a small tectonic plate (microplate) located off the coasts south of Panama and northwestern Colombia.It is named after Coiba, the largest island of Central America, just north of the plate offshore southern Panama.
The Panama block, a microplate, lies southeast of the country; its boundary with the Caribbean Plate, the Panama Thrust Bent, is a destructive plate boundary that stretches from Colombia to Limon, near the east coast of Costa Rica. In Costa Rica, the Panama Thrust Bent causes the Caribbean Plate to underthrust beneath the Cordillera de Talamanca.
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The northern boundary with the North American plate is a transform or strike-slip boundary that runs from the border area of Belize, Guatemala (Motagua Fault), and Honduras in Central America, eastward through the Cayman trough along the Swan Islands Transform Fault before joining the southern boundary of the Gonâve microplate.
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