SULAIY FORMATION SECTION (II)

 

Section 45 - Near lat 25°50' N.

 

[Generalized section of Sulaiy Formation near latitude 23°50' N., measurements by R.W. Powers and H.A. McClure, 1962]

 

Calcarenite of the Yamama Formation (Lower Cretaceous).

 

 

Thickness

Sulaiy Formation:

(meters)

 

Aphanitic limestone, golden-brown, tight, partially dolomitized ....................................................................

2.0

 

Pellet calcarenite, golden-brown, moderately sorted, medium- to coarse- grained, tightly cemented; abundant Foraminifera and pelecypod debris ……………………

1.8

 

Calcarenitic limestone, light-brown, moderately porous, chalky; 20 percent coarse-grained pelecypod and gastropod shell debris. Original shell material altered to clear, coarsely crystalline calcite. Lower 1.0-m-thick bed is tan aphanitic limestone. ………………….....................

3.2

 

Pellet calcarenite, tan, fine-grained, well-sorted, tightly cemented; abundant Foraminifera…………………….....

2.0

 

Aphanitic limestone, tan, moderately porous, chalky; very rare thin beds of brown, moderately porous, chalky pelecypod calcarenitic limestone….....….....…..........…..

35.5

Covered interval; thickness unknown ……………........

?

 

Aphanitic limestone, tan, moderately porous, chalky; thin beds of tan chalky, medium- to coarse - grained, pellet- molluscan calcarenitic limestone occur near top….........

5.1

 

Pellet calcarenite, dark-brown, well-sorted, fine-to medium-grained, tightly cemented; thin bed of tan chalky aphanitic limestone occurs in upper part………………...

4.0

 

Aphanitic limestone, tan, moderately porous, rarely pelletal; common outlines of monaxon sponge spicules. A 2.0-m-thick bed of brown, rarely sandy, chalky, pellet calcarenitic limestone occurs near middle………………...

5.5

 

Pellet calcarenite, golden-brown, well-sorted, very fine grained, tightly cemented……………………………...

1.5

 

Aphanitic limestone, tan, moderately porous, chalky; rare scattered molluscan debris and some sponge spicules. Occasional thin beds of brown tight, fine-medium-grained, pellet calcarenitic limestone…………………………...

14.5

Base of section probably near slump contact of Arab and Sulaiy Formations.

 


STEINEKE M. & BRAMKAMP R.A. [1952].- Geology of the Arabian Peninsula. Sedimentary Geology of Saudi Arabia. A review of the sedimentary geology of Saudi Arabia as shown on USGS Miscellaneous Geologic Investigations Map I-270 A, “Geologic Map of the Arabian Peninsula,” 1963. Geological Survey Professional Paper 560-D, Washington, 147 p.
From page D140.
Reprinted by courtesy of the U.S. Geological Survey, U.S. Department of the Interior.

Reprinted by courtesy of the U.S. Geological Survey, U.S. Department of the Interior