The Playa Hermosa Formation, Playa Verde Basin, Uruguay.

PAZOS, PABLO; RAPALINI, AUGUSTO E.; SANCHEZ BETTUCCI, LEDA; TOFALO, OFELIA R.

Geological society Memoir No.36 "The Geological Record of Neoproterozoic Glaciations"

Geological Society of London

Lugar: Bath; Año: 2011; p. 547 - 553

<!-- /* Font Definitions */ @font-face {font-family:"MS Mincho"; panose-1:2 2 6 9 4 2 5 8 3 4; mso-font-alt:"ＭＳ 明朝"; mso-font-charset:128; mso-generic-font-family:modern; mso-font-pitch:fixed; mso-font-signature:-536870145 1791491579 18 0 131231 0;} @font-face {font-family:"Cambria Math"; panose-1:2 4 5 3 5 4 6 3 2 4; mso-font-charset:0; mso-generic-font-family:roman; mso-font-pitch:variable; mso-font-signature:-1610611985 1107304683 0 0 159 0;} @font-face {font-family:Calibri; panose-1:2 15 5 2 2 2 4 3 2 4; mso-font-charset:0; mso-generic-font-family:swiss; mso-font-pitch:variable; mso-font-signature:-1610611985 1073750139 0 0 159 0;} @font-face {font-family:"@MS Mincho"; panose-1:2 2 6 9 4 2 5 8 3 4; mso-font-charset:128; mso-generic-font-family:modern; mso-font-pitch:fixed; mso-font-signature:-536870145 1791491579 18 0 131231 0;} /* Style Definitions */ p.MsoNormal, li.MsoNormal, div.MsoNormal {mso-style-unhide:no; mso-style-qformat:yes; mso-style-parent:""; margin-top:0in; margin-right:0in; margin-bottom:10.0pt; margin-left:0in; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:"Calibri","sans-serif"; mso-fareast-font-family:"MS Mincho"; mso-bidi-font-family:"Times New Roman"; mso-ansi-language:EN-GB;} .MsoChpDefault {mso-style-type:export-only; mso-default-props:yes; font-size:10.0pt; mso-ansi-font-size:10.0pt; mso-bidi-font-size:10.0pt; mso-ascii-font-family:Calibri; mso-fareast-font-family:"MS Mincho"; mso-hansi-font-family:Calibri;} @page Section1 {size:8.5in 11.0in; margin:1.0in 1.0in 1.0in 1.0in; mso-header-margin:.5in; mso-footer-margin:.5in; mso-paper-source:0;} div.Section1 {page:Section1;} --> The Playa Hermosa Formation is a volcano-sedimentary unit outcropping in the extreme south of the Dom Feliciano Belt in Uruguay. This unit was traditionally interpreted as not influenced by glacial processes until the interpretation of a glacial-related origin for the deposits in the lower part of the unit was suggested.  The stratigraphic position of the unit is subject of debate as well as its correlation with other Neoproterozoic units of Uruguay, Argentina and southern Brazil. Coeval sedimentation and volcanism provided the best constraints for its age suggesting circa 580 Ma for the contemporaneous magmatism using 39Ar/40Ar in hornblende, which is the best estimate for its sedimentation age. Preliminary paleomagnetic data from these sediments suggest a primary remanence for this unit and provide a mean geomagnetic pole consistent with the proposed apparent polar wander path for the Río de  la Plata craton. Although in need of confirmation, these data suggest that deposition of these glacigenic sediments may have occurred at low to intermediate latitudes. Future  research needs to be focused on absolute dating, reliable paleomagnetics and on a more accurate  interpretation of the geology and sedimentology of this and other Neoproterozoic units of the Río de  la Plata craton that are suitable for chemostratigraphy techniques and biostratigraphic approaches (e.g Arroyo del Soldado Group)