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Table 5 Estimated heat reserves (J/y) for each granitoid

From: Radiogenic heat production in granitoids from the Sierras de Córdoba, Argentina

Granitoid

Magmatic event

Erosion level+

Area (km2)

Measured thickness (km)

Estimated thickness* (km)

Reservoir volume (km3)

Mean QA (μJ/g/y)

Heat reservoir (J/y)

AB

Achalian

Top

2474.00

13.00?

9.79

24,225.08

386.97

2.51E + 16

AB1

Achalian

Top

2474.00

13.00?

9.79

24,225.08

46.04

2.99E + 15

CMP

Carboniferous

Top?

94.25

3.00

2.66

282.74

55.00

4.16E + 13

CAB

Achalian

Middle

421.17

2.42

1020.25

44.14

1.21E + 14

CAB2

Achalian

Middle

44.18

1.00

44.40

31.19

3.71E + 12

CAB3

Achalian

Middle

339.53

2.13

722.73

63.56

1.23E + 14

IGG

Achalian

Top

196.35

3.62

710.88

28.41

5.41E + 13

LoPP

Achalian

Top?

2.95

1.04

3.06

40.94

3.36E + 11

SP

Carboniferous

Top

23.25

1.99

46.35

44.11

5.72E + 12

LPP

Famatinian

Middle?

21.99

1.04

22.97

14.38

8.84E + 11

GP

Famatinian

Middle?

39.27

1.19

46.90

8.04

1.01E + 12

LFP

Famatinian

Middle?

18.85

0.88

16.57

5.15

2.28E + 11

SAP

Famatinian

Middle

1.96

0.52

1.02

3.10

8.47E + 09

Calmayo

Famatinian

Middle

8.58

0.80

0.71

El Hongo

Famatinian

Middle

10.8

0.8

0.69

La Yeya Sur

Achalian

Middle

4.12

0.5–1.0

0.64

  1. +The intrusions whose erosion level has been assigned with a question mark do not have information regarding their degree of erosion. In these cases, the erosion level is assigned according to their similarities with other nearby intrusions of the same magmatic event
  2. *Corrected for erosion. For details see Additional file 1: Table S2
  3. 1Without Bt-Ap-rich bodies samples
  4. 2Alpa Corral pluton
  5. 3El Talita pluton