Sample
|
Rock type
|
Igneous suite
|
Locality
|
206Pb/238U age ± 2σ
|
N
|
N*
|
MSWD
|
---|
DG063
|
Diorite
|
Ophiolite
|
Săvârşin
|
155.9 ± 2.54
|
47
|
39
|
1.3
|
DG064
|
Gabbro
|
Ophiolite
|
Săvârşin
|
157.7 ± 2.57
|
50
|
38
|
1.3
|
DG082
|
Gabbro
|
Ophiolite
|
Căzăneşti
|
158.2 ± 2.54
|
46
|
41
|
1.1
|
DG068
|
Gabbro
|
Ophiolite
|
Cerbia
|
158.9 ± 2.75
|
24
|
19
|
1.5
|
DG072
|
Granite
|
IAG
|
Cerbia
|
152.9 ± 2.49
|
34
|
25
|
1.1
|
DG081
|
Andesite
|
IAG
|
Birtin
|
154.5 ± 2.50
|
45
|
35
|
1.2
|
DG062
|
Granodiorite
|
IAG
|
Săvârşin
|
158.6 ± 2.52
|
41
|
25
|
2.3
|
DG067
|
Rhyolite
|
IAG
|
Săvârşin
|
155.0 ± 2.49
|
50
|
20
|
3.3
|
DG069
|
Granodiorite
|
IAG
|
Cerbia
|
154.8 ± 2.47
|
46
|
21
|
3.5
|
-
206Pb/238U ages are weighted average ages calculated with Isoplot 3.75 (Ludwig 2012). The total uncertainty of the ages is at 2σ level and comprises internal and propagated external errors. N number of zircons of the sample analysed; N* number of zircons used for the age calculation