Sato, A. M., & Llambías, E. J. (2017). Middle Triassic trachytic lava flows associated with coeval dyke swarm in the North Patagonian Massif: A postorogenic magmatism related to extensional collapse of the Gondwanide orogen.
Cita Chicago Style (17a ed.)Sato, Ana María, y Eduardo Jorge Llambías. Middle Triassic Trachytic Lava Flows Associated with Coeval Dyke Swarm in the North Patagonian Massif: A Postorogenic Magmatism Related to Extensional Collapse of the Gondwanide Orogen. 2017.
Cita MLA (8a ed.)Sato, Ana María, y Eduardo Jorge Llambías. Middle Triassic Trachytic Lava Flows Associated with Coeval Dyke Swarm in the North Patagonian Massif: A Postorogenic Magmatism Related to Extensional Collapse of the Gondwanide Orogen. 2017.
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