High-resolution sequence divisions and stratigraphic models of the Amu Darya right bank
Autor: | Zhuang Ruan, Chuanjie Cheng, Tongcui Guo, Hongjun Wang, Liangjie Zhang, Chongyang Wu, Muwei Cheng, Bingsong Yu |
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Rok vydání: | 2019 |
Předmět: |
geography
geography.geographical_feature_category 010504 meteorology & atmospheric sciences Carbonate platform Shoal Sedimentary basin Structural basin 010502 geochemistry & geophysics 01 natural sciences Paleontology Sequence (geology) Facies General Earth and Planetary Sciences Sequence stratigraphy Sedimentary rock Geology 0105 earth and related environmental sciences General Environmental Science |
Zdroj: | Arabian Journal of Geosciences. 12 |
ISSN: | 1866-7538 1866-7511 |
DOI: | 10.1007/s12517-019-4416-y |
Popis: | The Amu Darya Basin in Turkmenistan is a large petroliferous sedimentary basin. We analyzed the Callovian-Oxfordian succession of the Amu Darya right bank area based on Vail’s classic sequence stratigraphy and drill core, logging, seismic, thin-section petrographic, and geochemical data. We found that the Callovian-Oxfordian sequence can be divided into five third-order sequences (SQ1–SQ5) and 15 fourth-order sequences (sq1–sq15). A stratigraphic framework for the study area was newly established, based on these high-resolution sequence divisions. Two types of carbonate platform models were developed: (i) Callovian, in which the region was likely a ramp platform with a gradual slope to the east. It is mainly developedouter ramp and mid-ramp facies deposition which consists of micritic limestones, shoal grainstones, and reef limestones; (ii) Oxfordian, during which the region likely evolved into a rimmed platform with highly disparate sedimentation rates (low in the east) that were sensitive to sea level change, and a starkly different sedimentary landform that was high in the west and low in the east. |
Databáze: | OpenAIRE |
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