WebThe Motagua–Polochic fault system is particularly active ( Fig. 3), as evidenced by the great 1976 earthquake ( Ms =7.5) that ruptured a 230 km-long segment of the Motagua Fault ( … WebTraductions en contexte de "bien les séismes" en français-anglais avec Reverso Context : Les yourtes supportent bien les séismes.
Tectonic aspects of the guatemala earthquake of 4 february 1976
WebApr 1, 2024 · The largest seismically active faults are related to the transform, left-lateral, North America-Caribbean plate boundary zone, the most prominent of which are the Motagua and Polochic faults, both exceeding 350 km in length. Additionally, the Ixcán fault, a 150-200-km-long left-lateral structure, is located north of the Polochic and Motagua faults. WebNov 1, 2009 · We report results from a six-month seismological experiment in the area of the eastern Polochic-Motagua fault system (Guatemala) designed to both characterize the present seismicity and bring some constraints on the lithospheric structure. The seismic activity occurs in the upper 15 km of the crust, on the Polochic and the Motagua faults as ... the skimm investment round
High-pressure, metasomatic rocks along the Motagua Fault Zone ...
WebDownload scientific diagram The Motagua-Polochic fault zone. MF is the Mixco fault. GCG is the Guatemala City graben. TPF is the Tonalá-Polochic fault zone. LAF is the Los … WebTectonics. The Lowlands lie wholly within the Maya Block of the North American Plate. They notably house the Ticul Fault to the north, the Rio Hondo, Yucatán Channel, and Maya Mountain Faults to the east, and a portion of the Motagua–Polochic Fault Zone to the south. WebThe Motagua River of Guatemala follows the Motagua fault zone (MFZ), the present plate boundary zone between the North American (Maya block) and Caribbean (Chortís block) plates. The central Motagua River valley is bordered by E-W-striking tectonic slices of serpentinite, some of which contain blocks of high P/T eclogite, garnet the skimm fidelity investment