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1)  Liaodong
辽东
1.
Development and Declining of the Liaodong Economical Centre in the Regime of Mr.Gongsun;
公孙氏政权下辽东经济中心的发展与衰落
2.
On the Management and Exploitation in Liaodong by Yan State in the Warring States Period;
战国之燕对辽东的经营开发
3.
On the Influence to the Relationship of Nationality in Liaodong of Late Ming Dynasty by Traditional View between "Hua" and "Yi";
论传统华夷观对晚明辽东民族关系的影响
2)  eastern Liaoning
辽东
1.
A report of species characteristics of white craw duck in the eastern Liaoning;
辽东白嗉鸭种质性能研究报告
2.
Geochemistry and origin of tourmalite from boron-bearing rock series of Houxianyu borate deposit in eastern Liaoning;
辽东后仙峪硼矿床含硼岩系中电英岩的地球化学特征及其成因
3.
In order to reveal the nature and deep process of the Cenozoic lithospheric mantle in eastern North China Craton(NCC),the K-Ar dating,petro-geochemistry,and mineral chemistry of xenocrysts from the Caiyuanzi basalt in eastern Liaoning are studied in this paper.
通过对辽东菜园子玄武岩中的橄榄石和单斜辉石捕虏晶进行K-Ar定年及岩石地球化学测试,研究华北克拉通东部新生代岩石圈地幔的性质及深部作用过程,结果表明,辽东菜园子玄武岩形成于古近纪,K-Ar年龄为36。
3)  Eastern Liaoning Province
辽东
1.
Metallogenic Conditions of Magnesite and Talc Deposits in Early Proterozoic Mg-rich Carbonate Formations, Eastern Liaoning Province;
辽东早元古代富镁质碳酸盐岩建造菱镁矿和滑石矿床成矿条件
2.
A lot of large to giant magnesite and talc deposits located in Mg-rich carbonate formations distributed in the Paleoproterozoic Dashiqiao Formation in eastern Liaoning Province, China.
辽东地区古元古代大石桥组中分布有富镁质碳酸盐岩建造,并产有大型或超大型菱镁矿、滑石矿床。
3.
In the Paleoproterozoic Lieryu Formation and Dashiqiao Formation, eastern Liaoning Province, China, are distributed the magnesium rich carbonate rock formations, where occur large to super large sized deposits of borax, magnesite, talc, and serpentine.
辽东地区古元古代裂谷里尔峪组和大石桥组中分别分布有富镁质的碳酸盐岩建造 ,其中产有硼矿、菱镁矿、滑石、岫岩玉等大型 -特大型矿床 。
4)  Liao Dong
辽东
1.
Korea People Moving into Liao Dong District: Causes,Ways and Contribution to Development of this Land in Early Days of Ming Dynasty;
明前期朝鲜族移居辽东的原因、途径及开发贡献
5)  EastLiaoning
辽东
1.
ThePaleoproterozoicCratonRiftinEastLiaoningisagiantrift,whichdevelopedinArcheangranite-greenstoneterrainbythestretchingofthecrust.
辽东古元古宙克拉通裂谷是太古宙花岗岩绿岩地体受地壳的拉伸作用而形成的巨大裂谷带,西起郯庐断裂,向东经盖县、宽甸、桓仁进入吉林和朝鲜。
2.
Throughdeepstudiesanddiscussiononthegeological,lithologicalandgeochemicalcharacteristics,genesisandemplacementmechanismofpaleoproterozoicstreakgraniterocksinEastLiaoning,itisconsideredthatthegraniterocksareakindofcomplicatedrock,calledcrust-mantlemixedcomplex,whichformedfromapartlymeltenmassinamixedbedofthecrustandmantleduringthetransformingstagefromextensionalmechanismtocompressivemechanism.
辽东地区古元古代条痕状花岗质杂岩呈东西向展布于辽东古裂谷带中,侵入辽河群,最高可达大石桥岩组。
6)  East Liaodong area
辽东东地区
1.
A 2-D experiment model was used for modeling oil migration and accumulation in the East Liaodong area.
采用二维物理模型对辽东东地区石油运移和聚集进行了实验研究,结果证实:①断层带的石油运移方式对石油运移路径产生了重要的影响;②3套不整合面在不同充注方式下对石油的输导作用不同,馆陶组下段和东营组之间的不整合面(不整合面1)在2种充注方式下对石油都起到输导作用,东营组与沙河街组之间的不整合面(不整合面2)和沙河街组沙二段与沙河街组沙四段之间的不整合面(不整合面3)仅在幕式充注情况下对石油的运移起到侧向输导作用;③东营组砂体最终能否成藏,取决于砂体与其他输导体的匹配关系,其中与油源断层相沟通且尖灭的砂体最有利于形成岩性油藏。
补充资料:辽东
辽河以东的地区,就是辽宁的东部和南部。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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