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《Geological Review》 1989-01
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THE NADANHADA TERRANE IN HEILONGJIANG PROVINCE

Zhang Qinglong(Department of Geologyp Nanjing University, China)Mizutani Shinjino, Kojima Satoru (Department of Earth Sciences, Nagoya University, Japan)and Shao Ji'an(Department of Geology, Beijing University, China)  
On the basis of a comparison and analysis of various terranes on the continerntal margins of eastern China, the authors discuss the stratigraphic sequences and rock associations of the Mesozoic Nadanhada terrane in northeastern China. This terrane is composed of upper Paleozoic and Mesozoic pillow lavas, limestones, edded cherts, shales, siliceous shales and sandstones. Triassic and Jurassic radiolarian fossil are found in the bedded cherts and siliceous shales. Carboniferous and Permian limestone lenses are found in Erlianqiao, which occur as olistoliths, intercalated together with blocks of basic lavas in weakly sheared Triassic and Jurassic sandstones and shales. So they are considered to be Mesozoic olistotromic complex.
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