1、

The contact relationship between Silurian and Devonian is parallel unconformity.

泥盆系与志留系之间为平行不整合接触.

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2、

The hydrocarbon generation content in Lower Cambrian and Lower Silurian is up to 60 % ~80 % of total.

原始生烃量以下古生界为主,下寒武统和下志留统的生烃量约占总生烃量的60%~80%.

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3、

The discovery of the Silurian-Devonian oil and gas reservoir reveals a good exploration prospect.

塔里木盆地志留 - 泥盆系油气藏的发现,展示了志留-泥盆系良好的勘探潜力.

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4、

Silurian System in Tarim Basin is distributed in an area of about 23.

塔里木盆地志留系分布面积约23.

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5、

It changed to ancient land due vertical movement in the end of the Silurian.

南秦岭在早古生代是扬子板块的被动大陆边缘,在志留纪末曾因垂向隆升变为古陆.

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6、

A rift trough along Mianxian-Lueyang ophiolitic melange belt was formed from Ordovician to Silurian.

奥陶纪—志留纪大致沿勉略构造带形成南秦岭裂陷槽.

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7、

Porphyry mineralization, occurred in the Silurian Period, finally formed ore bodies.

晚期矿化发生于志留纪, 使矿床最终形成.

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8、

THE RETZIELLIDAE ( SILURIAN RIBBED IMPUNCTATE ATHYRIDIDINE BRACHIOPODS )

论志留纪的小莱采贝类——具壳线、无疹无窗贝族(腕足动物 )

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9、

Sq 1 , Sq 4, Sq 10 are three favorableexploratory sequence of the Silurian and Devonian in Tarim basin.

Sq1 、 Sq4、Sq10是塔里木盆地志留-泥盆系的三个有利勘探层序.

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10、

From the Early Silurian large scale of retrogression had begun accompanying the Late Caledonian movement.

晚加里东运动(始于早志留世)发生了大规模的海退.

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11、

Phases of secondary pore generation and dissolution mechanism: taking Silurian Asphaltic Sandstone in Central Tarim Basin as an example

次生孔隙形成期次与溶蚀机理&以塔中地区志留系沥青砂岩为例

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12、

Diagenesis data indicate that the Silurian asphaltic sandstones are the products of multiple fillings of hydrocarbon.

志留系沥青砂岩的成岩作用特征等资料证明,沥青砂岩的形成是烃类多期次注入的结果。

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13、

Late Silurian-Early Devonian bryozoans from Baytik mountain of Xinjiang

新疆北塔山晚志留&早泥盆世苔藓虫

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14、

Genetic types of Silurian basal conglomerate in Southern Guizhou

黔南志留系底砾岩成因类型

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15、

According to the gravel composition, distribution, occurrence features and sedimentary features, the Silurian basal conglomerate in southern Guizhou may be classified according to its genesis into the storm event sedimentary type, tide channel lag type, karst collapse type and beach accumulation type.

依据底砾岩的砾石成份、分布和产出特征,以及沉积特点等,把贵州南部志留系的底砾岩分为风暴事件沉积型、潮道滞流型、岩溶垮塌型及海滩堆积型四种成因类型。

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16、

A phasic alternation of marine biota from Late Ordovician to Early Silurian and the geological age of the Guanyinqiao formation

扬子区晚奥陶世到早志留世海洋生物群的阶段性更替及观音桥组的时代

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17、

The extensional fault systems are believed to be developed through the Cambrian, Ordovician, Early Silurian, Middle-Late Jurassic, and Paleogene.

伸展断裂系统发育于寒武纪、奥陶纪、早志留世、中-晚侏罗世和古近纪。

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