About Difficulty starting internal combustion rock drills in Cote d Ivoire
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6 FAQs about [Difficulty starting internal combustion rock drills in Cote d Ivoire]
Are Albian-stage source rocks in the Côte d'Ivoire basin seismic?
Seismic facies characteristics of Albian-stage source rocks in the Côte d’Ivoire Basin. In order to reflect the distribution characteristics of the predicted source rocks, some seismic lines were selected for comprehensive analysis.
What is the TOC of the Côte d'Ivoire basin?
From the center of the basin to the edge of the transition area, wells such P and X have TOC values of about 2 wt.%–3 wt.%. The source rocks in the central area of the basin are obviously better than those in the peripheral area. Figure 9. TOC calculation plane distribution of Lower-Cretaceous-Albian-stage source rocks in the Côte d’Ivoire Basin.
What tectonic changes occurred in the Côte d'Ivoire basin?
In the Early Cretaceous period, the South American plate and the African plate rotated apart , and the equatorial Atlantic split to form the Côte d’Ivoire Basin, which constitutes a typical transformational passive continental margin basin . The Côte d’Ivoire Basin has undergone three major stages of tectonic evolution [4, 10, 11, 12, 19]:
What type of rock is in the Côte d'Ivoire basin?
Previous studies have suggested that the Côte d’Ivoire Basin is mainly composed of three sets of source rocks: Aptian, Albian, and Cenomanian–Turonian. The Aptian-stage source rocks are mainly lacustrine shale, and the kerogen type is mainly type III, with an average TOC of 0.6 wt.%~2.6 wt.%.
What is the lithology of the Côte d'Ivoire basin?
The high-quality source rocks in the the Albian-stage of the Côte d’Ivoire Basin are characterized by a medium amplitude, a low frequency, and continuous, parallel–subparallel reflection. They have widely developed in a semi-deep–deep lake environments, and the lithology is mainly thick dark mudstone.
What are the three stages of tectonic evolution in the Côte d'Ivoire basin?
The Côte d’Ivoire Basin has undergone three major stages of tectonic evolution [4, 10, 11, 12, 19]: Early rift stage: early Cretaceous Berriasian–Barremian stage.
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