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- W2375620119 abstract "In view of these facts that there are many subdivision plans of the Jiufotang Formation of Western Liaoning and other related issues, the authors measured more than ten sections which was 106km in all. Using the basic principles of lithostratigraphy and sedimentology, five tuffaceous rocks marker beds or measures are distinguished from the Jiufotang Formation in the Kazuo Basin. The Jiufotang Formation is subdivided into four members bounded on the top of Marker Bed or Measure 1,2,4,5. Member 1 mainly consists of light-gray,off-white tuffaceous rocks, to which sandstone and conglomerate are high in proportion;Member 2 mainly consists of light-gray, dark-gray siltstone and mudstone with oil shale, sandstone and conglomerate in partial regions; Member 3 mainly consists of brown-gray pelitic siltstone and dark-gray, glaucous silty mudstone and is subdivided into two sub-members by Marker Bed or Measure 3, and the upper sub-member contains oil shale with great industry significance; Member 4 mainly consists of light-gray, off-white siltstone, yellow-gray sandstone and glaucous mudstone. On this basis, these conclusions are elaborated that the deposition of tuffaceous material concerned with volcanic events in origin leads to the death of massive organisms and syndepositional clastic rocks and argillaceous rocks rooting in different types of mother rocks have differences in color in different parts of the basin. Finally, it is discussed that if there is the Shahai Formation above the Jiufotang Formation and the issue of its bottom boundary." @default.
- W2375620119 created "2016-06-24" @default.
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- W2375620119 date "2009-01-01" @default.
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- W2375620119 title "SUBDIVISION OF THE JIUFOTANG FORMATION AND RELATED ISSUES IN THE KAZUO BASIN" @default.
- W2375620119 hasPublicationYear "2009" @default.
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