Paleomagnetic result of the Lower-Cretaceous from Luanping basin,Hebei Province and its tectonic implications*     

Zhiming  Sun  Zhenyu  Yang  Xinghua  Ma  Yue  Zhao 《中国科学:地球科学(英文版)》1998,41(2):43-50

A paleomagnetic study of about 95 samples from 16 sites sampled in the Early Cretaceous in Luanping basin in Hebei Province was reported. Stepwise thermal demagnetization was used to isolate magnetic components. Most samples have a characteristic direction with a high temperature component above 500°C. The tectonic-corrected data areD = 347.8°,I = 50.4°, α₉₅ = 7.l°, and the corresponding pole position is at 76.1°N, 346.3°E,with dp =6.4°,dm = 3.8°, paleolatitude λ = 31.1°N. This result indicates a counterclockwise post-Cretaceous rotation of 30.7° ±9.8° with respect to the stable Ordos basin in the west of North China Block, and a non-significant northward motion. This rotation could be related to local fault action or structural detachment, or regional NNW-NWWward motion and collision of Kula-Pacific plate with eastern China since the Early Cretaceous.

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松花江水下爆破孔施工技术          下载免费PDF全文

赵大军  徐龙献  陈宝义 《探矿工程》1998,(4):12-14

在东北严寒季节,在松花江上施工水下爆破孔。介绍了施工设备及施工平台,根据不同地层分别采用静压振动下套管护壁及潜孔锤钻进方法,设计了风路系统,改进了套管妆方法,并采取了科学的管理方法,取产好的效果。  相似文献   

The Variance of Mango‘s Light—Hydrocarbon Parameter K   总被引：1，自引：0，他引：1  

张春明  赵红静等 《中国地球化学学报》1998,17(2):148-151

The analyses of light hydrocarbons in oils from the Tarim Basin show that the Mango‘s parameter K is about unity except those oils trapped in the eastern part of the Tazhong (Central Tarim)Fault Uplift,The regular variance of K may indicates the accumulation and admixture of the oil populations in the eastern part of the Tazhong Fault Uplift.  相似文献   

地震折射和反射波联合勘探在桥址区工程勘察中的应用     

刘保金  赵成斌  孙振国  王琦  崔昭文 《物探与化探》1998,22(2):134-138

用浅层地震折射和反射联合勘探方法在京—沪高速公路沭河桥址区进行隐伏断层和层位划分探测试验。试验是在宽约300m的水面上进行的,采用ES-2401高分辨率数字地震仪和“五小二高”的工作方法,综合利用折射和反射波信息,提高地质推断解释的可靠性,探测试验取得了良好的效果。  相似文献   

Evolutionary events of Cainozoic Ostracoda of western Philippine Sea and paleoceanographical implications     

Zhao Quanhong  Robin Whatley 《中国科学D辑(英文版)》1998,41(3):282-289

The Oligocene ostracod fauna of IISDP Site 292 of the western Philippine Sea was marked by high density, diversity and origination, probably reflecting a favorable period for deep-sea Ostraroda; while the sharp decrease in dtmsity and diversity as well as the repeatedly occurring vxtinctions in thc. Neogene may indicate the deterioration in bottom-water environmcnts at that tlme. Five rriajor faunal changes have been recognized in terms of density, diversity and evolutionary artivity (origination and extinction), occurring in the earliest Oligocene (PI8), mid-Oligocene (P21), earliest Miocene (N4), early Middle Miocene (N8) and late Pliocene (N21). respectively. These changes in ostracod faunas are suggested to represent short-term events related to global paleoceanographical changes and to record the Cainozoic cooling history of the West Pacific Ocean and Philippine Sea deep-water. Project supported by the National Natural Science Foundation of China (Grant No. 49676287).  相似文献   

Paleomagnetic result of the Lower-Cretaceous from Luanping basin,Hebei Province and its tectonic implications*     

Sun Zhiming  Yang Zhenyu  Ma Xinghua  Zhao Yue 《中国科学D辑(英文版)》1998,41(2):43-50

A paleomagnetic study of about 95 samples from 16 sites sampled in the Early Cretaceous in Luanping basin in Hebei Province was reported. Stepwise thermal demagnetization was used to isolate magnetic components. Most samples have a characteristic direction with a high temperature component above 500°C. The tectonic-corrected data areD = 347.8°,I = 50.4°, α₉₅ = 7.l°, and the corresponding pole position is at 76.1°N, 346.3°E,with dp =6.4°,dm = 3.8°, paleolatitude λ = 31.1°N. This result indicates a counterclockwise post-Cretaceous rotation of 30.7° ±9.8° with respect to the stable Ordos basin in the west of North China Block, and a non-significant northward motion. This rotation could be related to local fault action or structural detachment, or regional NNW-NWWward motion and collision of Kula-Pacific plate with eastern China since the Early Cretaceous.  相似文献   

含硬包体试样在破裂孕育过程中波速场的变化   总被引：2，自引：2，他引：0  

王彬  胡毅力 《地震研究》1998,21(3):256-260

含硬包体混凝土试样在底面支撑侧面双轴加压至主破裂的情况下波速场的变化图象为：加压初期,试样上的纵波平均速度在４１７５～４６１５ｍ／ｓ之间变化,随着压力升高,出现小于４１７５ｍ／ｓ的低速区,但范围甚小,位置在两个包体之间。随后出现大于４６１５ｍ／ｓ的高速区,范围大致与包体位置一致。随着σ１的增加,低速区在逐渐变大,高速区逐步减小后又重新变大,高速区与低速区在平面上相互重叠,在空间上看,高速区被低速区包围着。临近主破裂时,低速区变小并逐步形成条带,高速区也变小,主要集中在靠近未来出现破裂的一个包体位置上。最终的破裂面出现在此高速区与低速条带交界附近,包体也局部破裂了。  相似文献   

我国首座卫星信道数字化地震台网落成   总被引：1，自引：0，他引：1  

赵永  王斌 《国际地震动态》1998,(9):18-21

文章较为详细地介绍了我国第一座卫星信道数字化地震观测台网各配套仪器的性能,使用环境及整套系统的运行情况和目前在地震观测中所起的作用。作者展望了该系统的发展前景及其对我国地震观测事业的影响。  相似文献   

二滩水电站地震遥测台网持续时间震级的研制   总被引：2，自引：0，他引：2  

赵珠  谢蓉华 《地震地磁观测与研究》1998,19(2):21-29

利用二滩水电站地震遥测台网的速度量和位移量观测记录,收集了震级ＭＬ为０．４￣５．４的４６０次地震（Δ〈２１０ｋｍ）的振动持续时间３５００多条,制作了该台网的持续时间震级公式和便查表。在方法上,不同于通常的按一次或两次曲线拟合,而采取计算机自动分段按折线拟合的方法,以阻尼最小二乘法完成其计算;在资料上,先分台制作８个子台的持续时间震级公式,在此基础上选择仪器、台基及公式中参数相近的子台,制作了适用于  相似文献   

地震触发响应系数动态图象扫描及华北近期地震危险区预测     

赵根模  杨港生 《华北地震科学》1998,16(4):10-16

从理论上讲,地震之间存在力学相关性,尤其是一个地震带内在临界状态,地震间相互作用增强。利用这种关系用地震触发响应系数扫描方法,可在一个强震发生后预测下次强震发生的地点。地震引起的就力场扰动包括静态、动态扰动,包括断层弹性位错,也有断层蠕动,可以有弹性地震波和粘弹性形变波的传播实现,有弹性变形,也有永久变形,有瞬间的,也有长久的效应等。这方面已提出好多种效应假说,多种效应共同作用的后果是一个。Ａｔ值  相似文献