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1)  Jiaodong and Luxi areas
胶东和鲁西地区
1.
Jiaodong and Luxi areas are separated by Yishu fault.
胶东和鲁西地区被沂沭断裂带所分隔 ,在中侏罗世末期 ,由于郯庐断裂带发生大规模左旋平移运动 ,二个地区最终拼合在一起。
2)  eastern Henan (Yu) and Southwest Shandong (Lu) area
豫东、鲁西南地区
3)  Luxi area
鲁西地区
1.
Comparative analysis of Meso-Cenozoic tectonic evolutions of the Jiyang and Linqing depressions and Luxi area;
济阳、临清坳陷及鲁西地区中新生代构造演化对比分析
2.
As showed by zinc SHRIMP chronometric age result of early Cambrian crystalline basememt in Luxi area,the forming age of Taishan group is in about 2750Ma.
近年来在鲁西地区早前寒武纪结晶基底进行锆石SHRIMP测年结果显示,泰山岩群形成年龄大约在2770~2750Ma。
3.
There are two Mesozoic magmatic activity periods in Luxi area.
鲁西地区中生代有2个岩浆活动时期,中侏罗世岩浆活动规模较小,形成铜石杂岩体,锆石SHRIMP U Pb年龄167。
4)  Western Shandong
鲁西地区
1.
Primitive euconodonts are extrmely abundant and varied in the Late Cambrian in western Shandong Province.
鲁西地区晚寒武世地层发育 ,产有数量丰富、分异度大的原始真牙形石分子 ,经笔者研究 ,建立了 2新属、2新种及 2未定种 Camconodontus rotundatus gen et sp。
5)  west of Shandong
鲁西地区
1.
Cambrian stratigraphy well developed in Luxi(west of Shandong),and their sedimentary records possesses cyclicity.
鲁西地区寒武纪地层发育较好,沉积记录具旋回性的特点。
2.
Since the seventh“fiveyearplan”,the regional geological survey with the scale of 1∶50,000 and 1∶200,000 in west of Shandong has been carried out, and the Mesozoic intrusives have been further studied, where Jinan, Tongshi,Bucun and Yinan superunits established.
“七五”以来,鲁西地区开展的1∶5万和1∶20万区调工作,对中生代侵入岩的研究逐步深入,建立了济南、铜石、埠村、沂南等超单元。
6)  Jiaoliao Luxi and Xuhuai area
胶辽鲁西徐淮地区
1.
According to study on rock property combination, palaeobio characteristics and sesmic event strata, Neoproterozoic strata in Jiaoliao Luxi and Xuhuai area can be multi-divided and contrasted as follows: Heishanguan formation and Erqingshan formation in Luxi area are conformity with Diaoyutai formation and Nanfen formation, while Baoshankou fomation can contrast with Nanfen formation.
依据岩性组合、古生物特征及地震事件层研究 ,对胶辽鲁西徐淮地区新元古代地层可作如下多重划分对比 :鲁西黑山官组、二青山组分别与辽东的钓鱼台组、南芬组相当 ,胶东豹山口组可与南芬组对比 ,它们同属青白口系。
补充资料:奉和鲁望渔具十五咏·舴艋
【诗文】:
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【出处】:
全唐诗:卷611-14
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