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Biostratigraphy in sequence stratigraphy (view source)
Revision as of 20:38, 26 February 2014
, 20:38, 26 February 2014→Stratigraphic distribution of onlap events
==Stratigraphic distribution of onlap events==
==Stratigraphic distribution of onlap events==
[[file:applied-paleontology_fig17-23.png|thumb|{{figure number|1}}Stratigraphic distribution of onlap events, tectonic episodes (“s”-shaped arrows), oceanic anoxic events (OAE), and “crises” of the shallow water biota (<span class="noglossary">BC</span>) in various parts of the world during part of the Mesozoic.<ref name=ch17r80 />]]
[[:file:applied-paleontology_fig17-23.png|Figure 1]] illustrates the stratigraphic distribution of onlap events, tectonic episodes (“s”-shaped arrows), oceanic anoxic events (OAE), and “crises” of the shallow water biota (<span class="noglossary">BC</span>) in various parts of the world during part of the Mesozoic.<ref name=ch17r80>Simo, J., A., T., Scott, R., W., Masse, J.-P., 1993, [http://archives.datapages.com/data/specpubs/carbona1/data/a044/a044/0001/0000/0001.htm Cretaceous carbonate platforms: an overview], in Simo, J., A., T., Scott, R., W., Masse, J.-P., eds., Cretaceous Carbonate Platforms: [http://store.aapg.org/detail.aspx?id=1188 AAPG Memoir 56], p. 1–14.</ref>) Landward is toward the right in each column.
[[:file:applied-paleontology_fig17-23.png|Figure 1]] illustrates the stratigraphic distribution of onlap events, tectonic episodes (“s”-shaped arrows), oceanic anoxic events (OAE), and “crises” of the shallow water biota (<span class="noglossary">BC</span>) in various parts of the world during part of the Mesozoic.<ref name=ch17r80>Simo, J., A., T., Scott, R., W., Masse, J.-P., 1993, [http://archives.datapages.com/data/specpubs/carbona1/data/a044/a044/0001/0000/0001.htm Cretaceous carbonate platforms: an overview], in Simo, J., A., T., Scott, R., W., Masse, J.-P., eds., Cretaceous Carbonate Platforms: [http://store.aapg.org/detail.aspx?id=1188 AAPG Memoir 56], p. 1–14.</ref>) Landward is toward the right in each column.