1) Luliang Basin
陆良盆地
1.
Sedimentary characteristics of nearshore subaqueous fan of Neogene Ciying Formation in Luliang basin.Yunnan;
云南陆良盆地新近系茨营组近岸水下扇沉积特征
2.
Luliang Basin is a typical representative of Tertiary sedimentary basins in Yunnan Province.
陆良盆地是云南省第三系沉积盆地的典型代表。
3.
Luliang Basin is a typical representative of the Tertiary sedimentary basins in Yunnan Province.
陆良盆地是云南第三系沉积盆地的典型代表。
2) foreland basin
前陆盆地
1.
Transporting conditions of faults required in formation of large and medium gas fields with high efficiency in foreland basin;
前陆盆地高效大中型气田形成的断裂输导条件
2.
Different origins of natural gas in secondary gas pool in Western Sichuan foreland basin;
川西前陆盆地次生气藏天然气来源追踪
3.
Overpressure compartment sealed by faults in Kuqa foreland basin;
库车前陆盆地断裂封存的超高压封存箱
3) shelf basin
陆架盆地
1.
Chimney structures in the shelf basin of East China Sea;
东海陆架盆地台北坳陷烟囱构造特征
2.
Exploration of subtle reservoirs in the northern shelf basins of South China Sea;
南海北部陆架盆地隐蔽油气藏勘探
3.
Non-structural reservoirs in northern shelf basins of South China Sea;
南海北部陆架盆地非构造油气藏
4) continental basin
陆相盆地
1.
Relationship between unconformity system and heterogeneous migration of petroleum in continental basins;
陆相盆地中不整合体系与油气的不均一性运移
2.
Application prospects of cross well seismic technique to continental basins;
井间地震技术在陆相盆地的应用前景
3.
Petroleum Geology and exploration prospects in the Cenezoic continental basins in the northern part of the Qinghai-Xizang Plateau;
青藏高原北部新生代陆相盆地石油地质条件及勘探前景
5) terrestrial basin
陆相盆地
1.
Discussio on"one divides into four"property of system domain for stratigraphic sequence of terrestrial basins of China and its advantages;
论中国陆相盆地地层层序体系域的可四分性及其优势
2.
In analysis of imaging stratigraphy for Cretaceous terrestrial basin in Xingjiang,in the light of modern stratigraphic theory,using analysis methods of sequence stratigraphy and tectonic sequence,the recognition marks of imaging sequence interfaces in remote sensing are built, and combined with 1∶50000 geological survey,the interpretating methods of imaging tectonic sequenc are discussed.
在信江白垩纪陆相盆地的影像地层分析中，以现代地层学理论为指导，运用层序地层和构造层序分析方法，建立了遥感影像层序界面识别标志，结合１∶５万地质填图，论述了影像构造层序的解译方法。
3.
On the basis of analyzing the present situation of exploration in fault depressions in terrestrial basins,the conception of generalized sag is proposed,such as the alar part of the steep belt in fault depressions,the major sag,and the mid-lower part of slope belts.
在分析陆相盆地断陷勘探现状的基础上,提出了广义的断陷洼槽区概念,主要包括断陷陡带(翼部)、主洼槽区、斜坡带中低部位。
6) inland basin
内陆盆地
1.
Discuss on the representative enrichment mechanism of groundwater in the front of mountain around Inland Basin;
西北内陆盆地山前带典型地下水赋存模式探讨
2.
Study on the distribution and balance of the salt in the inland basin;
内陆盆地的盐分布与平衡分析研究
3.
Vertical water cycle and its ecological effect in inland basins, Northwest China;
中国西北内陆盆地水分垂直循环及其生态学意义
补充资料：陆良大觉寺千佛塔
造型而言，陆良大觉寺干佛塔在云南佛塔中别无二例，其样式在全国佛塔中也较为罕见，这正是它特别吸引人的地方。
大觉寺干佛塔在陆良县城南真理街大觉寺内，因夺得名。此塔已有六七百年历史了。《陆良县志》载:"寺始建于元，重修于明万历……寺前面则建鼓钟，东偏则塔凌霄汉。"(程光祖《重修大觉寺小引》)。现除塔之外大觉寺建筑还有正殿、鼓楼等。塔立于正殿之左。
此塔为六角形7级砖石结构，高17.79米，塔基为方形石砌台座，四面辟有佛凳各一，靠内原有佛像，今己佚失。基座上建六角形塔身，由下至上逐层收分，每层6面，每面用砖块砌成大小相等的小方佛拿，层层堆积，面面相依，远看恍如一巨大的塔形蜂巢。佛拿内各镶有一块释迦牟尼印像砖，砖上佛祖身披袈装，双手垂膝，盘足跌坐莲台之上，面目慈祥，正参禅入定，头部漾出一道"佛光"，可谓宝相庄严。塔7层，每层又有若干层佛龛，共计1613龛佛，是名副其实的"千佛塔"。
塔顶之南向位置，有铜质迦楼罗(金鸡)振羽距足，雄姿勃发，当地人因此又称"金鸡塔"。
除《陆良县志》所载明万历之外，大觉寺历代均作过修复，最近的一次是1982年省人民政府拨专款维修的。为保存文物风貌，此次首先参照残存佛凳内的佛像砖，重新烧制补齐，使各矣均有佛像砖，其次将塔顶已残的迦楼罗换上新的，并将塔身刷成金黄色，远远望去，金光滔滔，照眼耀明，倍增华彩。
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