Erratum to: Contrib Mineral Petrol (2015) 170:28 DOI 10.1007/s00410-015-1184-x
We have reported erroneous coordinates for sample localities in the Electronic supplementary material of this article. To allow for accurate sample location, we indicate here the correct sample coordinates in WGS84 latitudes and longitudes.
The caption of Figure S1 in the Electronic supplementary material should therefore read correctly:
Figure S1: Polished rock slabs and map coordinates (WGS84, latitudes and longitudes in degrees, minutes and seconds; format dd°mmʹss.sʺ). Black bars = 5 cm.
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(a)
Marginal facies granodiorite (CB03): 45°56′15.2ʺ, 10°26′01.5ʺ
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(b)
Plagioclase quartz diorite (CB13): 45°56′27.9ʺ, 10°25′43.0ʺ
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(c)
Val Fredda tonalite (CB09): 45°56′24.4ʺ, 10°25′02.0ʺ
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(d)
Mattoni gabbro (CB04): 45°55′31.0ʺ, 10°24′37.3ʺ
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(e)
Cadino gabbro (CB05): 45°56′20.9ʺ, 10°24′56.7ʺ
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(f)
Pegmatite (Peg): 45°56′23.9ʺ, 10°24′55.8ʺ
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(g)
Mattoni gabbro (AD9): 45°55′57.2ʺ, 10°25′19.3ʺ
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(h)
Mattoni gabbro (CS23): 45°55′57.2ʺ, 10°25′19.4ʺ
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The online version of the original article can be found under doi:10.1007/s00410-015-1184-x.
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Broderick, C., Wotzlaw, J.F., Frick, D.A. et al. Erratum to: Linking the thermal evolution and emplacement history of an upper-crustal pluton to its lower-crustal roots using zircon geochronology and geochemistry (Southern Adamello Batholith, N. Italy). Contrib Mineral Petrol 171, 27 (2016). https://doi.org/10.1007/s00410-016-1240-1
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DOI: https://doi.org/10.1007/s00410-016-1240-1