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| last8 = Peral | first8 = L. G.
| 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
| 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
| year = 2008 | journal = [[Precambrian Research]] | volume = 167 | issue = 1 | pages = 150–170
| url = https://www.researchgate.net/profile/Lucia_Gomez-Peral/publication/235452013_Detrital_zircon_ages_of_Neoproterozoic_sedimentary_successions_in_Uruguay_and_Argentina_Insights_into_the_geological_evolution_of_the_R'io_de_la_Plata_Craton/links/0deec53204db42bf79000000.pdf | accessdate = January 2016
| url = https://www.researchgate.net/publication/235452013 | accessdate = January 2016
| doi = 10.1016/j.precamres.2008.07.006 | ref = harv}}</ref> Sarandí del Yí Shear Zone is marked as "SYSZ". To the east [[Sierra Ballena Shear Zone]] is marked as "SBSZ".]]
| doi = 10.1016/j.precamres.2008.07.006 | ref = harv}}</ref> Sarandí del Yí Shear Zone is marked as "SYSZ". To the east [[Sierra Ballena Shear Zone]] is marked as "SBSZ".]]
The '''Sarandí del Yí Shear Zone''' is a [[strike slip fault|strike slip]] [[shear zone]] in [[Uruguay]]. The shear zone has a NNW-SSE orientation and a [[Sinistral and dextral|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 [[Dyke swarm|Uruguayan dyke swarm]] to the west.<ref>{{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}}</ref>
The '''Sarandí del Yí Shear Zone''' is a [[strike slip fault|strike slip]] [[shear zone]] in [[Uruguay]]. The shear zone has a NNW-SSE orientation and a [[Sinistral and dextral|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 [[Dyke swarm|Uruguayan dyke swarm]] to the west.<ref>{{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}}</ref>

Revision as of 00:59, 14 March 2019

Shear zones and terranes in Uruguay after Gaucher et al., 2008.[1] Sarandí del Yí Shear Zone is marked as "SYSZ". To the east Sierra Ballena Shear Zone is marked as "SBSZ".

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 40 kilometres (25 mi) and truncates the Uruguayan dyke swarm to the west.[2]

References

  1. ^ Gaucher, C.; Finney, S. C.; Poiré, D. G.; Valencia, V. A.; Grove, M.; Blanco, G.; Pamoukaghlián, K.; Peral, L. G. (2008). "Detrital zircon ages of Neoproterozoic sedimentary successions in Uruguay and Argentina: insights into the geological evolution of the Río de la Plata Craton". Precambrian Research. 167 (1): 150–170. doi:10.1016/j.precamres.2008.07.006. Retrieved January 2016. {{cite journal}}: Check date values in: |accessdate= (help); Invalid |ref=harv (help)
  2. ^ Halls, Henry C.; Campal, Nestor; Davis, Don W; Bossi, Jorge (2001). "Magnetic studies and U–Pb geochronology of the Uruguayan dyke swarm, Rio de la Plata craton, Uruguay: paleomagnetic and economic implications". Journal of South American Earth Sciences. 14 (4). Elsevier: 349–361. doi:10.1016/s0895-9811(01)00031-1. Retrieved 15 December 2015.
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