Cambrian-Ordovician Sedimentary Environment of the Central Transition Belt between Cathaysia and Yangtze

Author:

Zheng Ning,Song Tianrui

Publisher

Elsevier BV

Reference26 articles.

1. Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication of ocean ridge activity;M Adachi;Sedimentary Geology,1986

2. Ordovician and Silurian seawater chemistry, sea level, and climate: A synopsis;M Axel;Palaeogeography, Palaeoclimatology, Palaeoecology,2010

3. Stable carbon isotope stratigraphy in the Ordovician of South China;M Axel;Palaeogeography, Palaeoclimatology, Palaeoecology,2011

4. Transport and deposition of mud in deep-water environments: Processes and stratigraphic implications;K Boulesteix;Sedimentology,2019

5. Carbon isotopes and event stratigraphy near the Ordovician-Silurian boundary;J X Fan;Palaeogeography, Palaeoclimatology, Palaeoecology,2009

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