Stable carbon and oxygen isotope data of Late Ediacaran stromatolites from a hypersaline environment in the Tarim Basin (NW China) and their reservoir potential

@article{Zhu2021StableCA,
  title={Stable carbon and oxygen isotope data of Late Ediacaran stromatolites from a hypersaline environment in the Tarim Basin (NW China) and their reservoir potential},
  author={Dongya Zhu and Quanyou Liu and Jingbin Wang and Qian Ding and Zhiliang He},
  journal={Facies},
  year={2021},
  volume={67}
}
The occurrence of Precambrian stromatolites is closely related to the ancient seawater composition and the evolution of life. It is also a potential oil and gas reservoir. In what kind of environment the stromatolites of the upper Ediacaran Qigebulak Formation in the Tarim Basin developed, and whether they constitute potential hydrocarbon reservoirs, remained unclear. Stromatolites occur in 1–5 m thick layers, interbedded with thrombolites and dolostones. Distinct stromatolite morphologies were… Expand
1 Citations
Recrystallization of dolostones in the Cambrian Xiaoerbrak Formation, Tarim Basin and possible link to reservoir development
  • Yinggang Zhang, Wenqing Pan, +4 authors Tao Yang
  • Marine and Petroleum Geology
  • 2021

References

SHOWING 1-10 OF 119 REFERENCES
The Paleoproterozoic fossil record: Implications for the evolution of the biosphere during Earth's middle-age
Abstract The Paleoproterozoic (2.5–1.6 Ga) Era is a decisive time in Earth and life history. The paleobiological record (microfossils, stromatolites, biomarkers and isotopes) illustrates theExpand
The palaeobiology and geochemistry of Precambrian hydrocarbon source rocks
Abstract Organic carbon productivity and formation of hydrocarbon source rocks during the Early Precambrian was almost exclusively the product of the growth of microbial mats. Indirect evidence ofExpand
3.43 billion-year-old stromatolite reef from the Pilbara Craton of western Australia: Ecosystem-scale insights to early life on Earth
Abstract The 3.43 billion-year-old Strelley Pool Chert, Pilbara Craton, Western Australia, contains compelling evidence of Early Archaean life in the form of kilometre-sized remnants of an ancientExpand
Stromatolite reef from the Early Archaean era of Australia
TLDR
A multi-kilometre-scale palaeontological and palaeoenvironmental study of the Strelley Pool Chert, in which the first morphotype-specific analysis of the structures within their palaioenvironment and refute contemporary abiogenic hypotheses for their formation are undertaken. Expand
Rare earth and trace elements of microbialites in Upper Jurassic coral- and sponge-microbialite reefs
Major, trace (Y, Zr, Pb, Th and U), rare earth element (REE) and Sm–Nd isotope analyses were carried out on microbialites and detrital carbonate sediments collected in Upper Jurassic coral- andExpand
A stable isotope study of microbial dolomite formation in the Coorong region, South Australia
Abstract The Coorong Region of South Australia is a classic location for the study of modern dolomite formation. A number of ephemeral lakes here contain dolomite, whilst other lakes in closeExpand
Characteristics and formation mechanisms of the unconformity-related paleokarst reservoirs in the Upper Sinian, Northwestern Tarim Basin, China
Abstract In the Late Sinian, the Tarim Basin experienced regional tectonic uplift and subaerial exposure. A regional unconformity was extensively distributed during the succession from the Sinian toExpand
Biostratigraphic and chemostratigraphic correlation of Neoproterozoic sedimentary successions: upper Tindir Group, northwestern Canada, as a test case.
Recent advances in Proterozoic micropaleontology and sedimentary isotope geochemistry suggest that improved interbasinal correlation of Neoproterozoic (1000-540 Ma) successions is possible. BecauseExpand
Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications.
The recent proliferation of stratigraphic studies of delta 13C variation in carbonates and organic C in later Neoproterozoic and basal Cambrian successions (approximately 850-530 Ma) indicates aExpand
Types of Fluid Alteration and Developing Mechanism of Deep Marine Carbonate Reservoirs
Accurate recognition of the types of alteration fluid and the development mechanisms are important concerns in studying deep marine carbonate reservoirs. Major fluid types, such as seawater, meteoricExpand
...
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4
5
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