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Geofluids
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2020
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Article
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Tab 1
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Research Article
Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary)
Table 1
Distribution of studied samples within the formations.
Formation
Well
Core number
Core thickness (m)
Number of thin sections
Number of samples
Number of clay mineral samples
Sandstones
Claystones and siltstones
Calcareous marls
Algyő
K1
c1, c2
29.9
14
11
3
8
Algyő
B1
c1
45.7
16
9
5
Szolnok
Szk1
c1
8
14
9
5
Szolnok
M7
c1, c2, c3, c4
36.8
31
22
9
7
Szolnok
M6
c1
9
14
10
4
Szolnok
Mcs1
c1
9
16
10
6
Endrőd
M7
c5, c6
18
18
12
6
4
Endrőd
M6
c2, c3
15
18
12
6
Endrőd
c2
6
19
14
5
Studied in detail.