古城奥陶系礁滩相岩性圈闭带和罗布泊奥陶系礁滩相构造—岩性复合圈闭带。
Gucheng Ordovician reef beach facies lithostratigraphic trap zone and Luobupo Ordovician reef beach facies structure-lithostratigraphic trap zone.
碳酸盐台地沉积体系又可进一步分为局限台地、开阔台地、台地边缘礁滩及缓坡等沉积相。
The carbonate platform sedimentary system is further divided into such facies as restricted platform, open platform, platform margin reef and ramp.
预测的苍溪礁滩相具有典型的进积型层序地层特征，在地震剖面上并且具有可靠的波组下拉现象。
The predicted Cangxi reef and shoal facies show the characteristics of typical progradational sequence stratigraphy with reliable push-down.
精细解释表明，此类丘状体是低倾角逆断层构造、斜坡滑塌堆积及浊积扇等非礁滩沉积体的地震响应。
The accurate interpretation shows that such domal bodies are the seismic reflections of non-reef-bank deposits of low angle thrust faults, slope slump accumulative zones and turbidite fans.
该三角洲沉积的特征是入海河流流速低而流量大，泥沙含量高而粒级细小，在三角洲前缘伴生有生物礁(滩)。
The river for building the delta was characterised by low velocity, high discharge, high concentration of fine clay and sand, and associated with reef (shoal) in delta front.
东沙隆起碳酸盐岩台地生物礁、滩油藏的勘探，是珠江口盆地（东部）重要的勘探领域之一。
The reef oil-gas pool in the carbonate platform of Dongsha Massif is one of the most important exploration directions.
该三角洲沉积的特征是入海河流流速低而流量大，泥沙含量高而粒级细小，在三角洲前缘伴生有生物礁(滩)。
The river for building the delta was characterized by low velocity, high discharge, high concentration of fine clay and sand, and associated with reef (shoal) in delta front.
长兴组礁、滩储层的储集空间多样，粒间孔、粒间溶孔、粒内溶孔及生物溶模孔为主要储集空间，局部层段溶洞、裂缝发育。
The reservoir spaces included inter-grain pores, dissolved inter-grain pores, dissolved intra-grain pores and mold pores of fossils. caves and fissures existed in some layers.
长兴组礁、滩储层的储集空间多样，粒间孔、粒间溶孔、粒内溶孔及生物溶模孔为主要储集空间，局部层段溶洞、裂缝发育。
The reservoir spaces included inter-grain pores, dissolved inter-grain pores, dissolved intra-grain pores and mold pores of fossils. caves and fissures existed in some layers.
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