期刊文献+
共找到3篇文章
< 1 >
每页显示 20 50 100
The bounding-surfaces record of a barrier spit from Huangqihai Lake,North China:implications for coastal barrier boundary hierarchy
1
作者 单新 于兴河 +3 位作者 peter d.clift 王天意 谭程鹏 金丽娜 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2016年第5期1097-1105,共9页
Ground-penetrating radar and trenching studies of a barrier spit on the north shore of Huangqihai Lake were made,that reveal important implications for the coastal washover barrier boundary hierarchy and interpretatio... Ground-penetrating radar and trenching studies of a barrier spit on the north shore of Huangqihai Lake were made,that reveal important implications for the coastal washover barrier boundary hierarchy and interpretations of this depositional record.A four-fold hierarchy bounding-surface model,representing different levels of impact and genesis,is defined.Each level of the hierarchy is enclosed by a distinct kind of surface characterized by different ground-penetrating radar reflection features,sedimentary characteristics(color,grain size,sorting,rounding and sedimentary structures) and origin.We suggest that this hierarchical model can be applied to any coastal washover barrier deposits. 展开更多
关键词 coastal barrier boundary hierarchy washover deposits ground-penetrating radar bounding surface Huangqihai Lake
下载PDF
地震地层分析揭示南海西南部沉积、岩浆和构造演化
2
作者 Lu Li peter d.clift +3 位作者 Hung The Nguyen 骆帅兵(翻译) 王笑雪(校对) 张莉(校对) 《海洋地质》 2020年第4期45-66,共22页
南海西南部代表了一个在海底扩张开始前就固结的大陆壳区域。在这里,我们编制了一个多道地震反射数据网格来描述在完全破裂之前大陆-海洋之间的转变。我们识别了一个主要的大陆块体,它被一个地壳过度伸展的盆地从陆架边缘分开。渐新世-... 南海西南部代表了一个在海底扩张开始前就固结的大陆壳区域。在这里,我们编制了一个多道地震反射数据网格来描述在完全破裂之前大陆-海洋之间的转变。我们识别了一个主要的大陆块体,它被一个地壳过度伸展的盆地从陆架边缘分开。渐新世-早中新世裂谷作用之后,在16 Ma之前发生了轻微的挤压和反转,可能与研究区域东部的危险区——一个大陆块体,与婆罗洲之间的碰撞有关。反转的时间支持了海底扩张一直持续到16 Ma左右的模式,而不是所说的在20 Ma时变得不活跃。在16Ma之前,该地区的外陆架边缘经历了抬升,更早以前其曾是沉积中心。在此之后,当该地区其余部分处于热沉降阶段时,其外陆架边缘继续伸展。裂谷后的岩浆活动以散布在盆地内部或边缘的海山(5~10 km宽)形式出现,其形成年代为晚中新世和上新世。它们与构造活动的任何阶段都没有明显的联系。在上新世,尽管缺少脆性断裂,但由于外陆架边缘的进一步反转,导致了重大的不整合。我们推测,这个时候的整个南海是一个散布岩浆活动更广泛模式的一部分。在5.3 Ma之后的上新世,研究区南部的陆架边缘出现了进积的斜形构造,在更新世则向北部和东部扩展。与此同时,外陆架边缘以南的海槽中充满了超过1.35 km的更新世沉积物。虽然我们预计大部分沉积物将来自湄公河,但我们也认为由Molengraaff河及其支流从婆罗洲和马来半岛带来的额外沉积物。 展开更多
关键词 地震地层学 伸展作用 反转 海山 陆坡地形
下载PDF
Evolution of the Yangtze River and its biodiversity 被引量:1
3
作者 Feng Chen Ge Xue +7 位作者 Yeke Wang Hucai Zhang peter d.clift Yaowu Xing Jun He James S.Albert Jun Chen Ping Xie 《The Innovation》 EI 2023年第3期20-22,共3页
Documenting the origins of megadiverse(sub)tropical aquatic ecosystems is an important goal for studies of evolution and ecology.Nonetheless,the geological and ecological establishment of the modern Yangtze River rema... Documenting the origins of megadiverse(sub)tropical aquatic ecosystems is an important goal for studies of evolution and ecology.Nonetheless,the geological and ecological establishment of the modern Yangtze River remains poorly understood.Here,we reconstruct the geographic and ecological history of an endemic clade of East Asian fishes based on the mitochondrial phylogenomics analysis of Cyprinidae using 15 fossil calibrations.We estimate an ancestral condition of benthic spawning with demersal or adhesive eggs in southern East Asia before23 Ma and a derived condition of riverine spawning with semibuoyant eggs in the Yangtze by18 Ma.These results imply the formation of Yangtze riverine ecosystems around the Oligocene-Miocene boundary in response to plateau uplift and monsoon strengthening.Some of these cyprinids reverted to benthic spawning with adhesive eggs by15 Ma,a time of rising to peak net diversification rates,indicating the formation of potamo-lacustrine ecosystems by the mid-Miocene during a strong East Asian summer monsoon.Our study provides increased spatiotemporal resolution for the co-evolutionary histories of the Yangtze River and its biodiversity and highlights biological evidence concerning the geomorphological dynamics of the Yangtze River. 展开更多
关键词 YANGTZE LACUSTRINE UPLIFT
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部