| 浙东隆起带与西南日本黑濑川构造带地质演化之比较 |
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| 引用本文： | 杨志坚.浙东隆起带与西南日本黑濑川构造带地质演化之比较[J].资源调查与环境,1992(1). |
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| 作者姓名： | 杨志坚 |
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| 作者单位： | 南京地质矿产研究所 |
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| 摘 要： | 浙东、闽北陈蔡群和建瓯群所构成的浙东隆起带,东延过东海后,与西南日本黑濑川构造带的寺野、肥后变质岩类连接,属“华夏—日本南方大陆”的北部残留地块,是受控于江山-绍兴-御荷(?)古断裂带而抬升暴露的.
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| 关 键 词： | 陈蔡群 寺野杂岩 浙东隆起带 黑濑川构造带 |
THE GEOLOGICAL EVOLUTION FEATURESCOMPARING BETWEEN EAST ZHEJIAN UPWARPING ZONE IN CHINA AND KUROSEGAWA TECTONIC ZONE IN SOUTHWEST JAPAN |
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| Yang Zhijian.THE GEOLOGICAL EVOLUTION FEATURESCOMPARING BETWEEN EAST ZHEJIAN UPWARPING ZONE IN CHINA AND KUROSEGAWA TECTONIC ZONE IN SOUTHWEST JAPAN[J].Resources Survey & Environment,1992(1). |
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| Authors: | Yang Zhijian |
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| Abstract: | The east Zhejiang upwarping zone, consisted of Chencai Group of east Zhejiang and Jianou Group of north Fujian in China, may be extended eastwards across the east China Sea and connected with the Jishino and Higo metamophic complex of Kurosegawa tectonic zone in southwest Japan, belonging to the north residual block of "Cathaysian-South Japan Continent" and controlled by Jianshan-Shaoxing-Mikabu Palaeofault.
The palaeotectonic evolution of east China, Korea Peninsula and southwest Japan was part of palaeo-Asia tectonic system trending in east to west. |
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| Keywords: | the east Zhejiang upwarping Zone Kurosegawa tectonic zone Chencai Group Jishino metamophic complex |
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