Table 2 Major and trace element concentrations of the diagenetic phases in the Cathedral Formation at Whirlpool Point, southern Rocky Mountains.

From: Shortwave infrared hyperspectral imaging as a novel method to elucidate multi-phase dolomitization, recrystallization, and cementation in carbonate sedimentary rocks

Phase

X-ray diffraction (XRD)

Inductively coupled plasma mass spectrometry (ICP-MS)

%Ca

Sr (ppm)

Fe (ppm)

Mn (ppm)

Replacement dolomite a (RDa)

XRD (n = 9)

  

ICP-MS (n = 5)

Min

49.27

24.7

958.0

38.6

Mean

50.21

171.3

2,407.1

182.7

Max

50.72

377.7

6,057.1

546.5

SD

0.471

167.8

2,097.6

212.7

Replacement dolomite b (RDb)

XRD (n = 12)

  

ICP-MS (n = 13)

Min

49.12

11.3

1444.5

101.4

Mean

49.79

18.1

4907.1

340.4

Max

50.30

37.5

11,006.0

813.3

SD

0.404

6.7

3649.7

218.3

Saddle dolomite (SD)

XRD (n = 17)

  

ICP-MS (n = 6)

Min

48.79

11.5

2026.1

183.6

Mean

49.65

20.2

7571.8

552.9

Max

50.57

26.8

12,290.0

813.6

SD

0.540

5.8

4272.9

278.4

Phase

Electron probe microanalysis (EPMA)

Ca (wt%)

Mg (wt%)

Fe (ppm)

Mn (ppm)

Saddle dolomite a (SDa)

Mean %Ca = 49.92

Min

15.92

8.42

0

0

Mean

21.07

12.82

2170

290

Max

26.22

16.46

4910

630

SD

2.209

1.751

1420

140

Saddle dolomite b (SDb)

Mean %Ca = 49.67

Min

16.13

8.85

0

0

Mean

21.06

12.94

3310

380

Max

25.99

17.03

5040

710

SD

2.202

1.744

1590

180

Saddle dolomite c (SDc)

Mean %Ca = 50.53

Min

14.77

7.53

0

0

Mean

20.45

12.14

12,130

1190

Max

26.13

16.75

36,740

2030

SD

2.261

1.822

2030

660

  1. %Ca = molar Ca/(Ca + Mg).