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南沙海域盆地群早中新世“挤压隆升幕”及其构造意义
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作者 关成尧 漆家福 +2 位作者 张厚和 廖宗宝 陈玮常 《地质科学》 CAS CSCD 北大核心 2022年第1期139-155,共17页
本文依据南沙海域实际地震测线资料,相关证据显示早中新世(T_(60)-T_(40)之间)南沙腹地多盆地发生挤压反转构造,南沙西南部多见挤压褶皱。南沙海域及周边地区在早中新世开始发生全区的挤压隆升和剥蚀,经过局部剥蚀量和构造抬升量定量估... 本文依据南沙海域实际地震测线资料,相关证据显示早中新世(T_(60)-T_(40)之间)南沙腹地多盆地发生挤压反转构造,南沙西南部多见挤压褶皱。南沙海域及周边地区在早中新世开始发生全区的挤压隆升和剥蚀,经过局部剥蚀量和构造抬升量定量估算,认为隆升核心区域的九章盆地由于挤压隆升导致的地层剥蚀量大于3 500 m。"早中新世挤压隆升幕"形成一个以郑和隆起为核心的"碟形"剥蚀区,活动时间与西南次海盆的扩张时间一致,西南次海盆的扩张可能是造成隆升幕的重要原因。由于隆升剥蚀前存在深埋,南沙腹地(九章盆地为代表)和南沙北缘(中业、永登盆地为代表)的"浅、薄、小"盆地群的价值不容忽视。 展开更多
关键词 南沙盆地 剥蚀 隆升幕 挤压 构造恢复 反转构造
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南沙曾母盆地地震反射特征 被引量:1
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作者 姚伯初 白志琳 《中国海上油气(地质)》 1992年第4期67-74,共8页
在曾母盆地地震反射剖面上解释出三个地震波组:T1、T2和T5(Tg),部分地区还存在T3波组。利用反射波的振幅、连续性、内部结构和外部形态,进行地震地层学解释,划分出三个反射层序。分析其地震反射波组特征、重力及磁力异常的特征,... 在曾母盆地地震反射剖面上解释出三个地震波组:T1、T2和T5(Tg),部分地区还存在T3波组。利用反射波的振幅、连续性、内部结构和外部形态,进行地震地层学解释,划分出三个反射层序。分析其地震反射波组特征、重力及磁力异常的特征,认为曾母盆地东北部的南薇南拗陷和北康台地属南沙地块,其余部分属加里曼丹地块,它们在始新世末至早渐新世缝合,曾母盆地是发育在这一缝合线附近的前陆盆地。从石油地质学的角度看,曾母盆地具理想的生储盖组合,可能是我国寻找油气资源的又一潜在的战略基地。 展开更多
关键词 南沙曾母盆地 地震反射特征 地震层序 沉积相 前陆盆地 油气勘探
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Soil Erosion under Different Land Use Types and Zones of Jinsha River Basin in Yunnan Province,China 被引量:13
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作者 YANGZisheng LIANGLuohui 《Journal of Mountain Science》 SCIE CSCD 2004年第1期46-56,共11页
Severe soil erosion in the middle and upper reaches of Yangtze River has been regarded as a major environmental problem. The on-site impact of soil erosion on agricultural production and the off-site impact on floods ... Severe soil erosion in the middle and upper reaches of Yangtze River has been regarded as a major environmental problem. The on-site impact of soil erosion on agricultural production and the off-site impact on floods and sedimentation in Yangtze Rive are well known. A quantitative assessment of soil erosion intensity is still scanty for developing appropriate soil erosion control measures for different land use types and zones in this region. This article constructs a localized USLE and estimates the average soil loss in the Jinsha River Region in Yunnan Province, one of the priority areas for soil erosion control in the middle and upper reaches of Yangtze River. The estimation is done under different land uses and zones in this basin. The estimation shows that while soil erosion in the cultivated land is the most severe, 36~40% of the garden and forest land suffers from soil erosion of various degrees due to lack of ground cover and other factors. Soil erosion in the pasture is modest when the ground cover is well maintained. It also confirmed that terracing can reduce soil erosion intensity significantly on the cultivated land. Research findings suggest that sufficient attention must be paid to regeneration of the ground cover in reforestation programs. In addition to mass reforestation efforts, restoration of grassland and terracing of the cultivated land should also play an important role in erosion control. 展开更多
关键词 Soil erosion soil loss equation land use type soil erosion control Jinsha River Basin in Yunnan
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