地台活化
- 网络platform activation
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同位素体系计时结果表明地幔交代作用是导致地台活化的先驱事件。
The timing result of isotopic systematies reveals that mantle metasomatism was a precursory event resulting in platform activation .
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坝区花岗岩体形成于地槽期,强烈改造于地台活化期。
The granite in dam site was formed in the period of the geosyncline and strongly reformed in the period of platform activation .
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地幔的的热侵蚀&中国东部大陆壳体后地台活化的一种深部过程
Lithospheric thermal erosion : a deep process of post-platform remobilization of eastern Chinese Lithosphere
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地台活化与栖霞山铅锌多金属矿床的形成
Activation of platform and the formation of the lead-zinc polymetallic ore deposits in Xi Xia mountain
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地台活化主要表现为燕山&喜山期构造和岩浆活动对原有地质构造和金矿化进行了强烈的改造。
The main activity of platform are that the original geological structure and Au were reformed intensely by Yanshan-Xishan period structure and magmatic activity .
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它既是华北地台活化的重要深部地质作用,亦是深部去根作用的具体体现。
It is not only an important deep geological process of North China platform activation but also the concret embodiment of deep " de-rooting " .
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中、新生代的地台活化期,长期受劳亚陆块、羌塘昌都陆块和扬子陆块不均匀的联合作用,构造热液活动复杂。
During the period of platform activation in Mesozoic era and Cenozoic era , the tectonic - hydrothermal activity is complex because of the uneven action of Laurasia long-term land mass , the Qiangtang-Qamdo land mass and Yangtze land mass .
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山东牟乳金矿带位于华北地台东缘活化区。
The Mouping - Rushan gold ore belt lies in the activated region on the eastern margin of the North China Craton .
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辽宁省地壳演化经历了太古宙古元古代基底形成、中元古代中三叠世地台盖层发展、中三叠世以后地台活化等发展阶段。
The crustal evolution in Liaoning Province has undergone multiple stages , in which the basement was formed in Archeozoic - Paleoproterozoic Era , platform cover was developed in Mesoproterozoic-Middle Triassic , and platform was mobiled of after Middle Triassic . The Nos.
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辽宁省位于华北地台北缘,其地质构造演化主要经历了地台基底形成(Ar-Pt1)、盖层沉积(Pt2-T2)、地台活化(T3以后)三个阶段。
Liaoning province is located on the northern borderland of North China Platform , which has mainly experienced three stages : the forming of platform basement ( Ar-Pt 1 ), the depositing of cover ( Pt 2-T 2 ), and the activizing of platform ( after T 3 ) .