1) Wan an basin
万安盆地
1.
The Wan an basin, located in the southwestern part of the South China Sea, belongs to a large scale pull-apart basin.
万安盆地位于万安断裂西侧 ,是一个大型的走滑拉张盆地 。
2.
Five-type traps, including compression, extension, sheal, gravity and strata-lithology, have been divided on studing the feature of different tectonic movements, seismic sequences and deposition property found in Wan an Basin, and the authors have modeled the evolu- tion relationship between them according to south and north sections, further,analyzed the genesis of traps.
本文在分析万安盆地地质构造特征、地层划分和沉积特征的基础上,将该盆地圈闭划分为压缩型、伸展型、剪切型三种构造类圈闭和重力、地层-岩性两种非构造型的圈闭,并选用南、北两条典型地震剖面模拟了典型类型的圈闭形成过程及其与构造运动之间的演化关系,可为寻找同类型含油气圈闭和研究构造演化史提供可靠依据。
3.
There are four types of hydrocarbon reservoirs which are hill trap with basement rock,fault block trap,anticlinal trap and lithological-stratigraphic trap with carbonate plat- form or reefs in Wan an basin.
万安盆地存在有基岩潜山型油气藏、断块型油气藏、生物礁岩隆型油气藏和背斜型油气藏四大类型。
2) Wan'an Basin
万安盆地
1.
Wan'an Basin is a Cenozoic petroliferous basin in South China Sea,with the maximum thickness of sediments from Upper Eocene to Quaternary up to 12,000m.
万安盆地位于我国南沙海域西南部 ,是一个新生代含油气盆地。
2.
The generating machenism and structural evolution of Wan'an basin is studied based on geological structure of its basement and stratigraphical distribution.
在充分了解万安盆地基底地质结构和地层发育特征的基础上,揭示了盆地的成因机制和地质构造演化史,探讨了盆地的油气地质特征及其在不同地区的差异,并初步确定了盆地的含油气远景。
3.
Wan'an basin is a large scale Cenozoic sedimentary basin which is located on southwest shelf of the South China Sea.
万安盆地是南海西南部陆架上的大型新生代沉积盆地。
4) Shiwanshan Basin
十万山盆地
1.
Shiwanshan basin has a Mesozoic to Cenozoic continental sedimentary cover lies over a basement of marine-facies Indosinian deformation.
十万山盆地是在印支期海相沉积基底上发育的中新生界陆相沉积盆地。
5) Qian an Basin
迁安盆地
1.
Vegetation changes and human influences on natural environments since 5 000 a BP were discussed based on the pollen data supported by radiocarbon dating from Cangumiao and Yujiawa profiles in Qian an Basin, the southern area of Yanshan Mountain.
依据位于燕山南部迁安盆地蚕姑庙村和余家洼村具放射性碳年代测定支持的埋藏泥炭剖面的孢粉分析资料 ,揭示了迁安盆地 5 0 0 0aBP以来自然植被变化和人类活动对自然环境的影响。
6) Anyuan Basin
安远盆地
1.
High-density Resistivity Surveying and the Features of Boundary Fault along the Edge of Anyuan Basin;
安远盆地边缘断层高密度电法探测及活动特征
补充资料：柏万安之母曹氏《善女人传》
【柏万安之母曹氏《善女人传》】
曹氏。常州柏万安之母也。年六十四。病热。万安自苏州驰归。视母气巳绝。唯胸前微温。家人治棺衾悉具。万安悲恸。祷于白衣大士。诵白衣咒一万二千。愿减巳寿一纪以益母。涕泪并下。其明日。索饮。阅数日。病起。言始死时。为两吏所引。历土地城隍诸司。寻诣东岳府。府君言。汝有子。为汝诚祷。仗大士力。贷汝死。命吏引出放还。万安遂勤母修净业。除一室。供佛像。曹氏遂长斋。日以初中后分入室。掏数珠。诵西方佛名辄千万计。居十二年。年七十六。九月既望。晨兴。谓其子曰。吾将去矣。可召诸亲属为别。明日亲属毕至。曹氏悉与款语。戒诸子女。临去明勿哭。日饮汤四五盏。至第三日昧旦。起坐。洗沐毕。易衣就枕而逝。事在乾隆三十三年
曹氏。常州柏万安之母也。年六十四。病热。万安自苏州驰归。视母气巳绝。唯胸前微温。家人治棺衾悉具。万安悲恸。祷于白衣大士。诵白衣咒一万二千。愿减巳寿一纪以益母。涕泪并下。其明日。索饮。阅数日。病起。言始死时。为两吏所引。历土地城隍诸司。寻诣东岳府。府君言。汝有子。为汝诚祷。仗大士力。贷汝死。命吏引出放还。万安遂勤母修净业。除一室。供佛像。曹氏遂长斋。日以初中后分入室。掏数珠。诵西方佛名辄千万计。居十二年。年七十六。九月既望。晨兴。谓其子曰。吾将去矣。可召诸亲属为别。明日亲属毕至。曹氏悉与款语。戒诸子女。临去明勿哭。日饮汤四五盏。至第三日昧旦。起坐。洗沐毕。易衣就枕而逝。事在乾隆三十三年
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