Titlebook: Latest Ordovician to Early Silurian Shale Gas Strata of the Yangtze Region, China; Xu Chen,Hongyan Wang,Daniel Goldman Book 2023 Zhejiang

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書目名稱Latest Ordovician to Early Silurian Shale Gas Strata of the Yangtze Region, China讀者反饋




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指數(shù)

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tooth-decay

978-981-99-3136-1Zhejiang University Press and Springer Nature Singapore Pte Ltd. 2023

航海太平洋

Introduction,ence stage, (2) exploration and appraisal stage, and (3) scale production construction stage. The graptolite zonation method was introduced at the Fuling Conference and immediately received full support by the SINOPEC, PetroChina and Geological Survey of China.

Estimable

Ordovician to Silurian Shale Gas-Bearing Strata from the Yangtze Region,er. These lithologic and biologic columns are the basic data for defining the Ordovician–Silurian shale gas-bearing strata correlation across the Yangtze Platform and its marginal belts, from which the distribution of most potential shale gas-bearing graptolite strata might be easily identified.

冒失

Palpitation

,Paleogeography and Paleoenvironment Across the Ordovician–Silurian Transition in the Yangtze Regionopach maps. Sedimentary processes during the Late Ordovician to early Silurian of the Yangtze Platform are reviewed. Microfacies analyses on the shale gas drill cores in Weiyuan and Luzhou are provided as additional data.

反饋

,Gamma Log Responses Through the Ordovician–Silurian Black Shale Graptolite Zonal Succession in the ing order: GR1 is located at the boundary of the Pagoda Formation and the Wufeng Formation; GR2 is located at LM1; GR3 is located within LM3–LM4 or is absent locally; and GR4 is located near the boundary of LM5 and LM6.

就職

Myosin

Geological Setting of the Ordovician and Silurian Strata of the Yangtze Platform,Boundaries separating different parts of the Yangtze Platform during the Ordovician and Silurian are defined on evidence of tectonic evolution. Constraint factors of distribution patterns, lithofacies, biofacies and the relationship with their surrounding units are provided.