1) Internal-tide deposits
内潮汐沉积
1.
Based on a comprehensive study of cores and various data, the authors considered that the sandstones and oolitic limestones in the Middle and Upper Ordovician of Well TZ32 in the Tarim Basin were mainly origin of internal-tide deposits.
这些特征表明砂岩和鲕粒灰岩为深水斜坡上的内潮汐沉积的产物。
2) Internal-tide deposit
内潮汐沉积
1.
Study on internal-wave and internal-tide deposits of the third member of the Lower Cambrian Balang Formation at Yangjiaping, Shimen;
石门杨家坪下寒武统杷榔组三段内波和内潮汐沉积研究
3) Inter-wave and inter-tide deposits
内波内潮汐沉积
4) tidal deposits
潮汐沉积
1.
Most of deposits of Zhuhai Formation are formed in tidal environment,and the main rock type is lithic subarkose;most of deposits of Lower Zhujiang Member are formed in shoreline environment,and the main rocks type is lithic arkose,and shoreline deposits with less mud,were well developed in western area;tidal deposits with more mud,were well developed in the eastern area.
以沉积学和高分辨率层序地层学理论为基础,通过薄片、扫描电镜观察、测井和地球化学分析等手段,对珠江口盆地惠州凹陷A区块珠江组下段和珠海组滨岸—潮汐沉积储层岩性和物性特征进行研究,该区珠海组以潮汐沉积为主,岩性主要为岩屑质长石砂岩;珠江组下段以滨岸沉积为主,岩性主要为岩屑质亚长石砂岩,西部滨岸沉积发育,岩性较纯,东部潮汐沉积发育,砂泥混杂。
5) lnternal-tide and internal-wave deposit
内潮汐和内波沉积
6) tidal silt deposit
潮汐粉沙沉积
补充资料：尾矿分散管及库内尾矿沉积滩
尾矿分散管及库内尾矿沉积滩
尾矿分散管及库内尾矿沉积滩
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条