Difference Analysis of Organic Matter Enrichment Mechanisms in Upper Ordovician-Lower Silurian Shale from the Yangtze Region of Southern China and Its Geological Significance in Shale Gas Exploration

<div>Sedimentary characteristics of the late Ordovician-early Silurian in southern China. The X-1 well is located in the upper Yangtze region, which is a deep-water shelf environment that is surrounded by ancient land; the Y-1 well is located in the lower Yangtze region, close to the junction of the Yangtze Plate and the Cathaysian Plate [<a href="/journals/geofluids/2019/9524507/#B24">24</a>, <a href="/journals/geofluids/2019/9524507/#B25">25</a>, <a href="/journals/geofluids/2019/9524507/#B29">29</a>].</div>

Geofluids

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Figure 1: Difference Analysis of Organic Matter Enrichment Mechanisms in Upper Ordovician-Lower Silurian Shale from the Yangtze Region of Southern China and Its Geological Significance in Shale Gas Exploration 

Figure 1 | Difference Analysis of Organic Matter Enrichment Mechanisms in Upper Ordovician-Lower Silurian Shale from the Yangtze Region of Southern China and Its Geological Significance in Shale Gas Exploration 