风暴沉积 meaning in Chinese
storm deposit
Examples
- Study of tempestite sedimentary of paleogene in huimin depression
惠民凹陷古近系风暴沉积研究 - The sequence is characterized by shallow - water proximal storm deposits
该风暴沉积具有原地或近原地特点。 - Comparisons of the sequence with those reported from the lower cambrian of northwestern hunan province as well as lower cambrian ooid banks of central guizhou province would be of much implication
该风暴沉积的发现，对建立与黔中和湘西北同期地层的沉积学对比剖面、探讨风暴沉积模式的空间变化具有重要意义。 - Sequence with features of proximal storm deposits associates closely with sequence with features of distal storm deposits at the longtangwan section , possibly resulting from differences in strength of storm fluids or in landing path of storm fluid
另外，不同的、类似于近源和远源的风暴沉积序列出露于同一剖面的相邻层位，可能反映了风暴登陆路径或者风暴流强度的差别。 - Typical sedimentary structures of tempestite , such as radiate and imbricate arrangements of strip dolomitic limestone gravels , grading beddings and ripple beddings are presented in the succession , indicating its accumulation in a shoreline environment
该风暴沉积的底面侵蚀构造清楚，长条形白云质灰岩砾屑具放射状构造或叠瓦状构造，并发育渠铸模、粒序层理和小型波状层理等沉积构造，为典型的浅水风暴岩。