奥连特盆地白垩系海绿石成因类型及沉积地质意义

阳孝法; 谢寅符; 张志伟; 马中振; 郭纯恩; 周玉冰; 王丹丹; 刘亚明; 赵永斌

doi:10.3799/dqkx.2016.501

Volume 41 Issue 10

Oct. 2016

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Article Navigation > Earth Science > 2016 > 41(10): 1696-1708

Yang Xiaofa, Xie Yinfu, Zhang Zhiwei, Ma Zhongzhen, Guo Chun'en, Zhou Yubing, Wang Dandan, Liu Yaming, Zhao Yongbin, 2016. Genetic Type and Sedimentary Geological Significance of Cretaceous Glauconite in Oriente Basin, Ecuador. Earth Science, 41(10): 1696-1708. doi: 10.3799/dqkx.2016.501

Citation:

Yang Xiaofa, Xie Yinfu, Zhang Zhiwei, Ma Zhongzhen, Guo Chun'en, Zhou Yubing, Wang Dandan, Liu Yaming, Zhao Yongbin, 2016. Genetic Type and Sedimentary Geological Significance of Cretaceous Glauconite in Oriente Basin, Ecuador. Earth Science, 41(10): 1696-1708. doi: 10.3799/dqkx.2016.501

Citation:

Yang Xiaofa, Xie Yinfu, Zhang Zhiwei, Ma Zhongzhen, Guo Chun'en, Zhou Yubing, Wang Dandan, Liu Yaming, Zhao Yongbin, 2016. Genetic Type and Sedimentary Geological Significance of Cretaceous Glauconite in Oriente Basin, Ecuador. Earth Science, 41(10): 1696-1708. doi: 10.3799/dqkx.2016.501

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Genetic Type and Sedimentary Geological Significance of Cretaceous Glauconite in Oriente Basin, Ecuador

doi: 10.3799/dqkx.2016.501

1.
Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
2.
CNPC America Ltd., PetroChina, Caracas 999188, Venezuela

Received Date: 2016-01-02
Publish Date: 2016-10-03

Abstract

Abstract

Glauconitic sandstones in Napo UT Member of Cretaceous developed widely in the Oriente Basin, Ecuador. Petrographic, mineralogical, geochemical, and spatial and temporal investigations of glauconite can reveal its composition, maturity, formation and genetic types, which, together with geological constraints, can better the understanding of the significance of sedimentary geology. Using the microscopy, X-ray diffraction (XRD), electron probe microanalyzer (EPMA) and Qemscan, petrography, mineral composition and major elements were analyzed systematically. Glauconite in UT Member shows dark green and curved rosette-like nanostructure and has high K₂O content (8 wt%), indicating it evolved to highly evolved and formed at low sedimentation rate in marine environment. Chemical composition and spatial and temporal attributes of glauconite reveal its characteristics of intrasequential (parautochthonous) glaucony, and indicate as well that it has undergone transport of storm surges and/or tidal currents processes. All evidences, including upward increasement of glauconite content, maturity variation, and similarity of morphology and chemical composition between samples from the outcrop and within the basin, indicate characteristics of parautochthonous glaucony. Upward increasement of glauconite content also suggests that the parautochthonous glauconite formed in the outer shelf shifted landward, indicating the relative sea-level rise during the marine transgressive setting. Widespread distribution of contemporaneous/para-contemporaneous glauconites usually represents the epeiric sea environment with stable tectonic setting.
- glauconite,
- mineralogy,
- geochemistry,
- sedimentary geology,
- Oriente basin

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Genetic Type and Sedimentary Geological Significance of Cretaceous Glauconite in Oriente Basin, Ecuador

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