Table 1. Mineralogy and stable isotopic composition of the diagenetic carbonates from the Cape Fear Diapir (Sites 991, 992, and 993) and from Blake Ridge (Sites 994, 995, and 997).
Core,
section, interval (cm) |
Depth (mbsf) |
In
situ temperature (ºC) |
Total carbonate (wt%) |
Dolomite d (104) (Å) |
![]() calcite ( ![]() |
![]() calcite ( ![]() |
![]() dolomite ( ![]() |
![]() dolomite ( ![]() |
![]() siderite ( ![]() |
![]() siderite ( ![]() |
![]() ( ![]() |
![]() ( ![]() |
---|---|---|---|---|---|---|---|---|---|---|---|---|
164-991A- |
||||||||||||
6H-1, 54-55 |
47.64 |
5 |
42.4 |
2.902 |
6.21 |
-27.82 |
0.5 |
|||||
6H-1, 56-57 |
47.66 |
5 |
2.902 |
6.19 |
-28.21 |
0.54 |
||||||
6H-1, 58-59 |
47.68 |
5 |
77.1 |
2.902 |
6.58 |
-31.22 |
0.91 |
|||||
6H-1, 63-64 |
47.73 |
5 |
59.8 |
2.902 |
6.75 |
-30.86 |
1.08 |
|||||
6H-3, 80-81 |
50.9 |
5 |
41.7 |
2.904 |
6.58 |
-31.26 |
0.91 |
|||||
164-992A- |
||||||||||||
2H-6, 59-61 |
10.89 |
4.5 |
56.8 |
2.902 |
6.27 |
-25.69 |
0.6 |
|||||
164-993A- |
||||||||||||
2X-3, 72-74 |
5.62 |
4 |
2.9 |
7.53 |
-20.77 |
1.85 |
||||||
2X-3, 88-91 |
5.78 |
4 |
n.d. |
7.44 |
-21.23 |
1.76 |
||||||
164-994C- |
||||||||||||
2H-1,47-48 |
4.87 |
4 |
24.4 |
2.887 |
1 |
0 |
-2.1 |
-4.6 |
-7.7 |
|||
4H-1,89-90 |
24.29 |
4 |
31.3 |
2.891 |
0.24 |
-0.1 |
-0.33 |
-1.88 |
-6 |
|||
6H-1, 26-27 |
42.66 |
4 |
27.6 |
2.889 |
0.18 |
0.22 |
-0.58 |
0.81 |
-6.2 |
|||
6H-4, 68-69 |
47.28 |
5 |
62 |
2.896 |
-3.74 |
-0.5 |
4.05 |
-9.08 |
-1.6 |
-6.4 |
||
7H-7, 20-21 |
61.1 |
5.5 |
13.2 |
2.891 |
-1.86 |
-0.43 |
-1.24 |
-2.12 |
-6.8 |
|||
10H-6, 97-98 |
80.37 |
6.5 |
63.8 |
2.898 |
-3.26 |
-0.35 |
4.8 |
-7.42 |
-0.57 |
-5.5 |
||
11H-4, 69-70 |
86.59 |
6.5 |
13.3 |
2.890 |
-0.47 |
-2.68 |
0.43 |
-7.8 |
||||
17H-1, 28-29 |
138.68 |
8.6 |
35.3 |
2.886 |
-4.56 |
-0.77 |
-2.23 |
1.66 |
-6.9 |
-6.2 |
||
20X-4, 2-3 |
162.92 |
9.5 |
20.6 |
0.38 |
0.35 |
3.31 |
7.81 |
-1.96 |
||||
26X-2, 75-76 |
215.15 |
11.4 |
10.1 |
0.79 |
-1.07 |
2.95 |
6.96 |
-1.83 |
||||
33X-3, 54-55 |
273.93 |
13.6 |
17.5 |
0.4 |
-0.03 |
2.57 |
5.2 |
-1.63 |
||||
40X-1, 82-83 |
329.12 |
15.6 |
16 |
0.3 |
-0.28 |
3.47 |
5.58 |
-0.26 |
||||
47X-2, 50-51 |
388.1 |
17.7 |
8.3 |
0.44 |
0.34 |
3.35 |
3.22 |
0.2 |
||||
52X-2, 86-88 |
426.86 |
19.1 |
27 |
0.55 |
0.29 |
2.65 |
5.37 |
-0.2 |
||||
57X-2, 64-65 |
464.9 |
20.5 |
17.5 |
-0.09 |
0.36 |
2.05 |
2.71 |
-0.32 |
||||
73X-4, 66-67 |
592.33 |
25 |
7.7 |
2.13 |
7.34 |
0.82 |
||||||
77X-1, 32-33 |
626.92 |
26.4 |
15.7 |
2.11 |
3.56 |
1.1 |
||||||
78X-1, 46-47 |
636.66 |
26.7 |
0.95 |
-0.76 |
3.4 |
5.2 |
2.38 |
|||||
78X-4, 133-134 |
641.55 |
27 |
13.1 |
0.29 |
0.17 |
2.32 |
1.74 |
1.4 |
||||
83X-3, 26-27 |
686.94 |
28.6 |
16.7 |
0.88 |
-1.55 |
1.85 |
2.22 |
1.33 |
||||
164-995A- |
||||||||||||
5H-4, 79-80 |
35.49 |
4.8 |
-1.25 |
-2.28 |
1.07 |
-9.48 |
-4.6 |
|||||
6H-1, 137-138 |
41.07 |
5 |
67.9 |
2.898 |
-2.54 |
-0.92 |
6.07 |
-10.21 |
0.39 |
-5.2 |
||
6H-3, 25-26 |
42.95 |
5 |
65 |
2.896 |
-4.38 |
-0.76 |
4.06 |
-7.39 |
-1.6 |
-7 |
||
81X-6, 84-85 |
684.04 |
26.5 |
1.61 |
-3.03 |
2.7 |
3.82 |
1.68 |
|||||
164-997A- |
||||||||||||
5H-CC, 21-22 |
41.19 |
5.9 |
67.39 |
2.898 |
-1.71 |
-1.3 |
4.14 |
-8.44 |
-1.33 |
|||
7H-1, 100-101 |
51.4 |
5.3 |
49.06 |
2.898 |
-1.39 |
-0.45 |
0.97 |
-9.22 |
-4.57 |
|||
8H-3, 17-18 |
56.07 |
5.5 |
69.72 |
2.897 |
-1.63 |
0.4 |
6.49 |
-6.74 |
0.92 |
|||
8H-5, 45-47 |
59.4 |
5.6 |
25.82 |
2.897 |
3.23 |
-5.85 |
-1.45 |
|||||
13H-8, 72-73 |
109.6 |
8 |
39.9 |
2.896 |
-4.65 |
-0.47 |
-1.2 |
3.98 |
-6.2 |
-6.5 |
||
164-997B- |
||||||||||||
22X-1, 126-127 |
551.06 |
23.7 |
5.05 |
4.56 |
3.45 |
|||||||
46X-3, 119-121 |
734.43 |
27 |
4.85 |
5.90 |
3.9 |
Notes: In situ
temperatures have been deduced from the downhole measurements (Paull, Matsumoto,
Wallace, et al., 1996). The 18O values of dolomite and siderite have
been corrected for the differential phosphoric acid fractionation (Sharma and
Clayton, 1965; Carothers et al., 1988). The 18O
values of the diagenetic waters in equilibrium with the diagenetic dolomite,
siderite, and calcite have been deduced from the 18O values of the
carbonates and from the
values calculated for the in situ temperatures.