13.01.2015 Views

Surgil ESIA Report - Volume III - EKN

Surgil ESIA Report - Volume III - EKN

Surgil ESIA Report - Volume III - EKN

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

“O’ZLITINEFTGAZ” PC<br />

PFS “<strong>Surgil</strong> field complex costruction with valuable<br />

components retrieval”<br />

Palaeocene section - P 1 . The palaeocene deposits are presented in the bottom part by<br />

greenish-grey clay limestone, and in top by brownish marls with the numerous residues of<br />

inoserams, shells of urchins, fish scales and concretions of pyrite. Thickness of the<br />

palaeocene deposits is 10m.<br />

Eocene section - P 2. The deposits are presented by greenish-grey, and in the top part<br />

of the cross-section – by brownish-grey marls, dense, strong with the fauna residues,<br />

phytodetritus and fine-air pyrite. There are interlayers of writing chalk among marls.<br />

Oligocene section - P 3 . The cross-section of Oligocene age is composed of clays of<br />

the sea genesis, bedded conformability on the Eocene deposits. The clays are greenish-grey,<br />

marly in the bottom part of the cross-section with the fauna residues and fish scales, with<br />

inclusions of fine-air pyrite; the clays are green in the top part with tints of blue with<br />

interlayers of siltstones, sands and mudstones, with concretions of pyrite. The clay of<br />

Oligocene are low- permeable (1.5-2.0m/darcy), values of porosity reach 25%.<br />

The start of sediment accumulation was marked by extensive transgression of the sea.<br />

The same conditions, with short-term uplift of separate parts of territory, remained at<br />

accumulation of the Eocene deposits. The high sea regime was stabilized in Oligocene time.<br />

Thickness of the Palaeogene deposits is 548-632m.<br />

Quarternary system-Q.<br />

The Neogene deposits are absent and rocks of quarternary age with washout are<br />

bedded on the chalk and Palaeogene deposits of different ages.<br />

The quarternary deposits are presented by brownish-yellow, quartz-feldspar sands<br />

and loose sandstones, siltstones and grey loams. The sediment accumulation of the<br />

quarternary deposits occurred in alluvial-lake facial conditions with short-term<br />

transgressions of the sea. Thickness of the quarternary deposits fluctuates within 60-186m.<br />

<strong>Volume</strong> 2. Part 1. EIS Project for <strong>Surgil</strong> field construction<br />

24

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!