Table 2. Sources and attributes of porosity-permeability data sets. | ||||||||||||
No. | Authors | Sandstone | Grain | Sorting | Primary | Secondary | Depositional | Facies | Thin Section | Vitrinite | Maximum | Maximum |
Class** | Size | Minerals | Minerals | Environment | Porosity | Reflectance | Porosity | Permeability | ||||
1 | Aase and others, 1996 | SA to AK | Y | N | N | Y | N | N | N | N | 27.9 | 2620.0 |
2 | Amthor and Okkerman, 1998 | LA | Y | N | N | N | Y | N | Y | N | 28.0 | 2700.0 |
3 | Atkinson and others, 1990 | LA | N | N | N | N | Y | N | N | N | 30.8 | 7762.0 |
4 | Bloch and others, 1990 | SL | Y | N | N | N | N | N | N | N | 27.2 | 3981.1 |
5 | Bloch, 1991 | SL to QA | Y | Y | Y | N | Y | N | N | N | 19.4 | 2976.0 |
6 | Bloch and others, 2002 | na | N | N | N | N | N | N | N | N | 25.6 | 1412 |
7 | Bourbie and Zinszner, 1985 | QA | N | N | N | N | N | N | N | N | 28.5 | 7762.5 |
8 | Bowker and Jackson, 1989 | SA | N | N | N | N | N | Y | N | N | 18.2 | 173.8 |
9 | Cant and Ethier, 1984 | Conglomerate | N | N | N | N | N | Y | N | N | 11.6 | 2000.0 |
10 | Castle and Burns, 1998 | QA, SA, SL | N | N | N | N | N | N | N | N | 16.1 | 158.5 |
11 | Cazier and others, 1995 | QA | N | N | N | N | N | N | N | N | 12.0 | 616.0 |
12 | Chowdhury and Noble, 1992 | SA | N | N | N | N | N | Y | N | N | 19.7 | 93.3 |
13 | Clark and Reinson, 1990 | LA, SL, QA | Y | Y | N | N | N | Y | N | N | 22.0 | 955.0 |
14 | Corcoran and others, 1994 | SA | N | N | N | N | N | N | N | N | 34.7 | 1990.0 |
15 | Cox and others, 1994 | SA | N | N | N | N | N | N | N | N | 20.6 | 55.0 |
16 | Dickinson, 1996 | SA | N | N | N | N | N | Y | N | N | 31.2 | 199.5 |
17 | Dolly and Mullarkey, 1996 | na | Y | N | N | N | N | N | N | N | 21.1 | 22500.0 |
18 | Dolly and Mullarkey, 1996 | na | Y | N | N | N | N | N | N | N | 20.3 | 2051.0 |
19 | Dolly and Mullarkey, 1996 | na | Y | N | N | N | N | N | N | N | 29.6 | 56.0 |
20 | Dolly and Mullarkey, 1996 | na | Y | N | N | N | N | N | N | N | 23.7 | 25.0 |
21 | Dutton and Willis, 1998 | QA | N | N | N | N | N | N | N | N | 13.3 | 89.1 |
22 | Dutton and others, 2003 | AK | N | N | N | N | N | N | N | N | 30.6 | 249.0 |
23 | Ehrenberg, 1990 | SA | N | N | N | Y | N | N | Y | Y | 34.3 | 13451.0 |
24 | Estes-Jackson and others, 2001 | SL to LA | N | N | N | Y | N | Y | N | N | 22.4 | 4.3 |
25 | Ganer, 1985 | QA | Y | N | N | N | N | N | N | N | 16.9 | 416.9 |
26 | Gaupp and others, 1993 | QA, SA, SL, LA | N | N | N | N | N | Y | N | N | 21.0 | 100.0 |
27 | Grau, 2000 | QA | Y | N | Y | Y | N | Y | Y | N | 28.3 | 7980.0 |
28 | Grigsby and others, 1992 | QA to LA | N | N | N | Y | N | N | N | N | 16.0 | 7.8 |
29 | Hall and Link, 1990 | PC | N | N | N | N | Y | N | N | N | 37.0 | 1445.0 |
30 | Hirst and others, 2001 | QA | N | N | N | N | N | N | N | N | 20.1 | 251.9 |
31 | Hogg and others, 1996 | AK | Y | N | N | N | N | N | N | N | 26.7 | 8912.5 |
32 | Hosseini and Hayatdavoudi, 1986 | LA to SL | Y | Y | Y | Y | N | N | Y | N | 31.2 | 193.0 |
33 | Keighin and others, 1989 | varied | N | N | N | N | N | N | N | Y | 22.1 | 44.0 |
34 | Keighin and others, 1993 | FL | Y | Y | Y | N | Y | N | Y | N | 19.7 | 59.3 |
35 | Kerr and others, 1999 | na | Y | N | N | N | Y | Y | N | N | 23.8 | 407.4 |
36 | Langford and others, 1990 | FL | N | N | N | N | N | Y | N | N | 20.5 | 2.9 |
37 | Lindquist, 1988 | SA | N | N | N | N | Y | Y | N | N | 19.5 | 810.0 |
38 | Luffel and others, 1991 | QA | N | N | N | N | N | N | N | N | 17.2 | 75.9 |
39 | Mancini et al., 1990 | SA | N | N | N | N | Y | N | N | N | 16.9 | 234.4 |
40 | Marzano, 1988 | PC | N | N | N | N | N | Y | N | N | 42.9 | 5370.3 |
41 | Miller and Groth, 1990 | QA | Y | N | N | N | Y | N | N | N | 18.0 | 316.0 |
42 | Miller and others, 1990 | PC | Y | N | N | N | N | Y | N | N | 40.6 | 10000.0 |
43 | Mitchell-Tapping, 1997 | SL | N | N | N | N | N | Y | N | N | 18.5 | 182.0 |
44 | Montgomery, 1997 | na | N | N | N | N | N | N | N | N | 20.6 | 19.1 |
45 | Montgomery and Morrison, 1999 | QA | N | N | N | N | N | N | N | N | 13.9 | 100.0 |
46 | Montgomery and Leetaru, 2000 | QA to SA | N | N | N | N | N | N | N | N | 23.0 | 239.8 |
47 | Morgan and others, 1977 | QA | N | N | N | N | N | N | N | N | 22.5 | 758.8 |
48 | Morse, 2001 | QA | Y | N | N | Y | N | N | Y | N | 19.8 | 250.0 |
49 | Muller and Coalson, 1989 | SL | N | N | N | Y | Y | N | N | N | 22.2 | 630.9 |
50 | Newman, 1999 | na | N | N | N | N | N | Y | N | N | 25.2 | 1995.3 |
51 | Paul and others, 1976 | na | Y | N | N | N | N | N | N | N | 32.9 | 1631.0 |
52 | Pryor, 1973 | na | N | N | N | N | N | N | N | N | 57.0 | 149000.0 |
53 | Reedy and Pepper, 1996 | SA | N | N | N | N | N | N | N | N | 38.0 | 6310.0 |
54 | Shade and Hansen, 1992 | AK | N | N | N | Y | N | N | N | N | 14.5 | 7.8 |
55 | Shenhav, 1971 | na | Y | N | N | Y | N | N | N | N | 29.8 | 2000.0 |
56 | Smith, 1985 | SA | Y | N | N | N | N | N | N | N | 22.5 | 851.1 |
57 | Smith, 1985 | QA | Y | N | N | N | N | N | N | N | 28.8 | 1258.9 |
58 | Smith, 1985 | QA to SA | Y | N | N | N | N | N | N | N | 28.5 | 1621.8 |
59 | Sneider and others, 1977 | na | Y | N | N | N | N | N | N | N | 24.2 | 524.8 |
60 | Soeder and Randolph, 1987 | FL | N | N | N | N | Y | N | N | N | 11.5 | 1.0 |
61 | Spain, 1992 | SA | N | N | N | N | Y | N | N | N | 29.5 | 169.8 |
62 | Stiles and Hutfilz, 1992 | quartzofeldspathic | N | N | N | N | N | N | N | N | 27.4 | 3235.9 |
63 | Stricklin, 1999 | na | Y | N | N | N | Y | N | N | N | 22.4 | 1215.0 |
64 | Taylor and Soule, 1993 | AK | N | N | N | N | N | Y | N | N | 19.1 | 281.8 |
65 | Thomson, 1978 | QA | Y | N | N | N | N | N | N | N | 15.3 | 180.0 |
66 | Thomson and Stancliffe, 1990 | FL | N | N | N | Y | Y | N | N | N | 21.9 | 89.1 |
67 | Tillman and Martinsen, 1987 | na | N | N | N | N | N | Y | N | N | 17.7 | 94.0 |
68 | Trevena and Clark, 1986 | SL | N | N | N | N | N | N | N | N | 27.5 | 3000.0 |
69 | Wendlandt and Bhuyan,1990 | varied | N | N | N | N | N | N | N | N | 23.3 | 1393.6 |
70 | Worden and others, 2000 | SL & LA | N | N | N | N | N | N | Y | N | 19.6 | 158.5 |
*Lithology key | ||||||||||||
QA Quartz Arenite | SA Subarkose | |||||||||||
SL Sublitharenite | AK Arkose | |||||||||||
FL Feldspathic Litharenite | LA Litharenite | |||||||||||
(no data classed as lithic arkoses) | ||||||||||||
na not available |
U. S. Geological Survey Open-file Report 03-420