1) Dalongkou Formation

大龙口组
1.
Neoproterozoic Seismic Catastrophic Events in Dalongkou Formation of Central Yunnan and Their Geological Significance
滇中中元古界大龙口组地震灾变事件及地质意义
2) Dalongkou

大龙口
1.
Paleomagnetic Properties of Non-marine Permo-Triassic Transitional Succession of the Dalongkou Section, Jimsar, Xinjiang;
新疆吉木萨尔大龙口非海相二叠系—三叠系界线层段古地磁特征
2.
Through ostracoda biostratigraphical investigation on the continental Permo—Triassic transition suc- cession from the south limb of the Dalongkou anticline section in Jimsar,Xinjian found very abundant ostracoda fos- sils in the Guodikeng Formation.
通过对新疆吉木萨尔大龙口背斜南翼剖面,陆相二叠系—三叠系界线层段锅底坑组介形虫生物地层的研究,发现介形虫化石非常丰富,计有3属51种,可明显地划分为两个组合带,即①Panxiania reticulata -Darwinuloides circulosa-Darwinula parallela 组合带和② Darwinula rotundata-Darwinula gloria-Darwinula pseudooblonga 组合带。
3) west Dalongkou

西大龙口
1.
Therefore,the west Dalongkou is an ideal site for establishment of continental Permo-Triassic boundary stratotype.
新疆西大龙口二叠-三叠系界线剖面,露头优良,交通便利,构造简单,层序清楚,地层连续,特别是其中的古生物化石,门类繁多,成为研究和建立陆相二叠-三叠系界线层型的理想地区。
4) DLK of Xinjiang

新疆大龙口
5) Dalongkou Region

大龙口地区
1.
Structure modeling of Dalongkou Region in southern margin of Junggar Basin

准噶尔盆地南缘大龙口地区构造建模
6) Dawenkou group

大汶口组
补充资料:龙口
1.指龙形香炉的出烟口。 2.五龙口之省称。山东省莱阳市东南有五龙山,五龙山有水道五,于山下合流入海。五龙口即此五条水道汇聚入海处。 3.大坝未合龙时的流水口。
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