| 词条 | Sarandí del Yí Shear Zone |
| 释义 |
The Sarandí del Yí Shear Zone is a strike slip shear zone in Uruguay. The shear zone has a NNW-SSE orientation and a dextral relative direction. It runs across the Río de la Plata Craton from the coast east of Montevideo in the south to the town of Sarandí del Yí. Sarandí del Yí Shear Zone shows a relative displacement of {{convert|40|km|mi}} and truncates the Uruguayan dyke swarm to the west.[2] References{{portal|Geology|Precambrian|Uruguay|Prehistory of South America}}1. ^{{Cite journal | last1 = Gaucher | first1 = C. | last2 = Finney | first2 = S. C. | last3 = Poiré | first3 = D. G. | last4 = Valencia | first4 = V. A. | last5 = Grove | first5 = M. | last6 = Blanco | first6 = G. | last7 = Pamoukaghlián | first7 = K. | last8 = Peral | first8 = L. G. | title = Detrital zircon ages of Neoproterozoic sedimentary successions in Uruguay and Argentina: insights into the geological evolution of the Río de la Plata Craton | year = 2008 | journal = Precambrian Research | volume = 167 | issue = 1 | pages = 150–170 | url = https://www.researchgate.net/publication/235452013 | accessdate = January 2016 | doi = 10.1016/j.precamres.2008.07.006 | ref = harv}} {{Major South American geological formations}}{{DEFAULTSORT:Sarandi del Yi Shear Zone}}2. ^{{cite journal |last=Halls |first=Henry C. |last2=Campal |first2=Nestor|last3=Davis |first3=Don W|last4=Bossi |first4=Jorge |date=2001 |title=Magnetic studies and U–Pb geochronology of the Uruguayan dyke swarm, Rio de la Plata craton, Uruguay: paleomagnetic and economic implications |url=http://www.sciencedirect.com/science/article/pii/S0895981101000311 |journal=Journal of South American Earth Sciences |publisher=Elsevier |volume=14 |issue=4 |pages=349–361 |doi= 10.1016/s0895-9811(01)00031-1|access-date=15 December 2015}} 3 : Geology of Uruguay|Strike-slip faults|Precambrian South America |
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