1979
DOI: 10.1080/00206818209467050
|View full text |Cite
|
Sign up to set email alerts
|

Geologic structure and possible petroleum prospects of the Middle Caspian region

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
2
0

Year Published

2022
2022
2022
2022

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…Wireline logs and lithological summaries of wells penetrating the entire Red Series onshore, with basic lithological interpretations, are available in Soviet-era publications, the authors of which had very limited knowledge of fluvial processes or systems. Geodekyan et al (1962), for example, presented a panel of seven wells between the Cheleken field in the west (Fig. 13) and well Balaishem-2 about 150 km to the east, showing an eastward decrease in thickness accompanied by an increase in sand content.…”
Section: Onshore Western Turkmenistanmentioning
confidence: 99%
See 1 more Smart Citation
“…Wireline logs and lithological summaries of wells penetrating the entire Red Series onshore, with basic lithological interpretations, are available in Soviet-era publications, the authors of which had very limited knowledge of fluvial processes or systems. Geodekyan et al (1962), for example, presented a panel of seven wells between the Cheleken field in the west (Fig. 13) and well Balaishem-2 about 150 km to the east, showing an eastward decrease in thickness accompanied by an increase in sand content.…”
Section: Onshore Western Turkmenistanmentioning
confidence: 99%
“…Ince et al (2008) briefly described surface exposures on the Cheleken Peninsula which they interpreted as representing well-defined, sand-filled channels encased by floodplain deposits comprising reddened mudstones and thinly-bedded sandstones, although they give no indication of the nature of these channels. Within a well drilled on the Monzhukly outcrop, Geodekyan et al (1962) illustrated the Red Series as reduced to around 2000 m but dominated by sandstones and conglomerates; and farther east at Balaishem-2, they indicated that it is only around 1000 m thick, but again dominated by sandstones and conglomerates with an interval at the base, around 150 m thick, of "limestones" with subordinate sandstones and siltstones. No detailed information on the depositional environments is provided in Soviet-era publications beyond general descriptions of a "deltaiccoastal" environment.…”
Section: Onshore Western Turkmenistanmentioning
confidence: 99%