陆棚沉积 meaning in Chinese
shelf deposit
Examples
- Six lithofacies palaeogeographic maps of doushantuo , dengying , qiongzhusi , canglangpu , and longwangmiao ages of late sinian and early cambrian have been made in the light of dominant facies and in the way to make stratigraphic map
中扬子地区上震旦统发育了从碳酸盐潮坪、开阔台地、浅滩、台地边缘、斜坡到台地前缘盆地等沉积，下寒武统下部主要?细碎屑岩和碳酸盐岩组成的混合型浅海陆棚沉积，上部变成碳酸盐潮坪、开阔台地、台缘斜坡和台缘盆地沉积。 - Sedimentary environment in benxi stage from east to west were respectively shallow - sea muddied continental shelf , barrier island , lagoon and tidal flat . most area in taiyuan stage was distributed by shallow - sea continental shelf , but the northern and southeastern part were scattered by clastic tidal flat and carbonate tidal flat . sedimentary environment in shanxi stage , in the middle and late shihezi stage was deltas and lake
马5晚期研究区发育蒸发台地相和局限台地相；本溪期自东而西发育浅海泥质陆棚、障壁岛、泻湖及潮坪相；太原期大部分地区发育浅海陆棚沉积，北部和西南部则发育碎屑岩潮坪和碳酸盐潮坪沉积；山西期和石盒子中晚期为三角洲和湖泊沉积环境；石盒子早期广泛发育辫状河三角洲和湖泊沉积。 - The lower paleozoic continent marginal sedimentary strata in the north kunlun massif are sinian - cambrian alajiaoyi group and ordovician pishigaisayi formation . the former is composed of high maturity flysch deposit , the later consist of continental shelf deposit such as carbonate and slate and sandstone . these rocks implies that they might form at passive continental margin
与其曼于特蛇绿岩相关的早古生代边缘沉积岩在昆北地块上为震旦?寒武系阿拉叫依岩群、奥陶系皮什盖萨依岩组，前者为一套成熟度较高的陆源碎屑复理石沉积，后者为碳酸盐岩和含碳板岩砂岩等陆棚沉积，显示其具被动陆缘性质。