1887

Abstract

The evaluation of oil and gas generation potential of all series of the Jurassic system has been accomplished based on geochemical investigation of outcrop samples from the Svalbard and Franz-Josef Land Archipelagoes and core samples from the Barents Sea wells. Besides the already proven Upper Jurassic source rocks, the shaly interlayers within the Lower-Middle Jurassic strata with considerable concentrations of the organic matter have been identified. In the SE part of the Barents Sea these rocks have good source rock properties. The Lower-Middle Jurassic shalestones from the northern Archipelagoes are characterized by low hydrocarbon index and generation potential and cannot be considered as source rocks. The authors tried to determine regularities in changes of kerogen type, generation potential and maturity of organic matter in the Jurassic rocks

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20143147
2012-09-10
2024-04-25
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20143147
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error