![Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang, Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,](https://journals.sagepub.com/cms/10.1177/0144598717736630/asset/images/large/10.1177_0144598717736630-fig11.jpeg)
Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,
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Ordovician deep dolomite reservoirs in the intracratonic Ordos Basin, China: Depositional model and Diagenetic evolution - Anqing Chen, Shenglin Xu, Shuai Yang, Hongde Chen, Zhongtang Su, Yijiang Zhong, Sihan Hu, 2018
![Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang, Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,](https://journals.sagepub.com/cms/10.1177/0144598717736630/asset/images/large/10.1177_0144598717736630-fig7.jpeg)
Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,
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![Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang, Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,](https://journals.sagepub.com/cms/10.1177/0144598717736630/asset/images/large/10.1177_0144598717736630-fig4.jpeg)
Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,
![Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang, Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,](https://journals.sagepub.com/cms/10.1177/0144598717736630/asset/images/large/10.1177_0144598717736630-fig1.jpeg)
Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,
![Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang, Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment – An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin - Dongya Zhu, Dianwei Zhang,](https://journals.sagepub.com/cms/10.1177/0144598717736630/asset/images/large/10.1177_0144598717736630-fig10.jpeg)