Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Ruiji Cao"'
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 220:89-117
A well-preserved benthic, epifaunal assemblage of articulated sponges is described from the stone coal beds of the Lower Cambrian Hetang Formation at Lantian, southern Anhui Province, South China. These sponges are Meishucunian–Qiongzhusian (=Diand
Publikováno v:
29th Conference on Precision Electromagnetic Measurements (CPEM 2014).
Publikováno v:
Precambrian Research. 107:253-263
We report an unusual instance of macrofossil pyritization in the Precambrian: three-dimensionally pyritized internal molds of chuarids from the late Neoproterozoic Lantian formation (∼550–600 Ma) in southern Anhui Province, South China. These chu
Publikováno v:
2012 Conference on Precision electromagnetic Measurements.
This paper describes the development of the high voltage ac energy meter which is easier to install and maintain and have lower self power consumption. The energy meter covers the voltage range up to 10 kV and current range up to 100 A. The expand un
Autor:
Ruiji Cao
Publikováno v:
Precambrian Research. 52:167-178
The mat-ministromatolite bioherms from the Proterozoic Wumishan Formation exhibit three orders of cyclic growth patterns. The growth cycle can be interpreted in terms of daily, monthly and seasonal periodicities. Mat-ministromatolite bioherms used as
Akademický článek
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Publikováno v:
2012 Conference on Precision Electromagnetic Measurements; 1/ 1/2012, p1-24, 24p
Publikováno v:
2012 Conference on Precision Electromagnetic Measurements; 1/ 1/2012, p1-29, 29p
Autor:
Xiumian Hu
This book provides diversified and comprehensive sedimentary, stratigraphic, and paleontological information services in China both for scientific research and educational purposes. Although China has the largest number of 11 “golden nails” profi
Autor:
Vinod Tewari, Joseph Seckbach
STROMATOLITES: Interaction of Microbes with Sediments provides an overview and latest information about the formation of Stromatolites as a result of interaction of microbes with sediments. Eighty-three expert scientists from twenty-seven countries p