利用背景噪声校正海底地震仪钟差     

P.Gouédard  T.Seher  J.J.McGuire  J.A.Collins  R.D.van der Hilst  雷晨 《世界地震译丛》2018,(5)

地震记录中时间的精确性对于现代处理技术至关重要。然而,对于由无法直接通信的仪器组成的台阵来说,仪器之间的时钟同步是很困难的。通过全球定位系统(GPS)进行时间同步是陆上的一个选择,但不能用于水下测量,因为电磁信号在水中不能有效传播。如果时钟漂移是线性的,那么可以通过部署前后的全球定位系统同步来估计海底地震仪的时间校正。但对于很多应用来说,这还不够,因为在长时间的实验中,这种漂移的非线性部分可以达到数十到数百毫秒。我们提出两种技术方法来提取同步记录的海底仪器在部署完成之后的时间记录差异。这两种技术都是基于对地震背景噪声的互相关分析,即使时钟漂移是非线性的,也都是有效的。第一种称为时间对称性分析(TSA),易于应用但需要合适的解释,以使噪声互相关函数在时间上是对称的;第二种基于重复地震分析方法,没有这种限制。本文分别讨论了两种方法的优缺点。通过在两组海底地震仪数据集的实际应用,表明两种方法都可以将仪器时钟同步误差控制到约5ms以下(主周期的百分之几)。  相似文献   

综合地震和地质数据获得的坎特伯雷地震序列的震级—频度分布模型     

M.W.Stirling  F.R.Zuniga  杨国栋  张苏平 《世界地震译丛》2018,(6)

我们综合地质和地震数据获得了坎特伯雷地震序列的震级—频度分布模型。在确定分布曲线时,借机用新的数据解决了文献中的一个长期争议:对于断层或断裂带的地震活动性,究竟是古登堡—里克特关系还是特征地震模型描述得更好。结果表明,对于坎特伯雷地震序列的整个复合断裂带而言,若综合考虑古登堡—里克特曲线(拟合仪器目录数据)误差和格林代尔断层上大(主)震根据古地震推断的复发周期界限,震级—频度分布可用古登堡—里克特关系很好地描述。相反,对于格林代尔断层的较小区域,震级—频度分布用特征地震模型描述得更好。不同的就是尺度,因为坎特伯雷地震序列所代表的复合断裂带表现为古登堡—里克特分布,而该断裂带内的单个断层表现为特征地震分布。因此,地震风险模拟中震级—频度分布的确定必须考虑尺度因素,而不能简单地认为一条震级—频度分布曲线适用于所有断层情形。  相似文献   

Mineralogical and Fluid Characteristics of the Fluorite-rich Monakoff and E1 Cu-Au Deposits, Cloncurry Region, Queensland, Australia: Implications for Regional F-Ba-rich IOCG Mineralization     

David A. HOLWELL  Megan R. WILLIAMS  Richard M. LILLY  Iain MCDONALD 《《地质学报》英文版》2014,88(Z2):350-351

Please?refer?to?the?attachment(s)?for?more?details.  相似文献   

Gold Mineralization in the Eastern Tannu-Ola Ore District of the Altai-Sayan Folded Area (Russia)     

A.I.Chernykh 《《地质学报》英文版》2014,88(Z2):679-680

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General Aspects and Resource Potential of Uranium Deposits in China     

LI Ziying  ZHANG Jindai  CAI Yuqi  GUO Q. Y.  ZHU P. F. 《《地质学报》英文版》2014,88(Z2):1371-1372

Please?refer?to?the?attachment(s)?for?more?details.  相似文献   

Chromite in the Mantle Section of the Oman Ophiolite: Implications for the Tectonic Evolution of the Oman Ophiolite     

SAVELYEVA G.N.  BATANOVA V.G. 《《地质学报》英文版》2015,89(Z2):77-78

<正>Structure and composition of the Uralian ophiolites reflect a large spectrum of geodynamic environment of their creation during Paleozoic time:from mid-ocean ridge,rift zone in continental margin,and suprasubduction spreading zone(SSZ)with resultant lherzolite or harzburgite ophiolite type(LOT and HOT).Residual  相似文献   

Regolith Geochemical Studies in Kimberlitic Terrain: A Case Study from Lattavaram Kimberlite Cluster, Eastern Dharwar Craton, Southern India     

P. Ramesh CHANDRA PHANI 《《地质学报》英文版》2016,90(Z1):191-191

正Utility of geochemistry in mineral exploration is known since more than half-a-century.In reconnaissance diamond exploration,regolith geochemistry is a well known tool worldwide and helps in distinguishing bedrock  相似文献   

Quantitative morphometric analysis of the Jama River profile in a tectonically active margin (Northwestern Ecuador)     

Pedro S.B.REYES  Mauricio E.VALAREZO  Jenry CóRDOVA  Fran?ois A.MICHAUD  Camilo ZAPATA 《山地科学学报》2018,15(5):966-975

The longitudinal profile of a river channel can be described in function of mathematical expressions. The logarithmic fit is the most used method to describe the relative equilibrium of a channel elevation profile. Rivers showing zones of high channel gradient and convex-upward profiles can be evaluated in function of the offset distance with respect to the logarithmic curve. The Jama River profile has been constructed using differential GPS data for the downstream reach and 4-m-grid DEM data base for the remaining headward profile. The resulting longitudinal profile shows a prominent knickpoint of about 80 m in elevation characterized by sharp local convexity. The offset distance in vertical direction from the logarithmic plot is interpreted as the successive accumulation of multiple uplift episodes associated with the Jama Fault System activity. The horizontal offset is suggested to represent the remaining retreated distance for the upstream propagation of the Jama knickpoint. The highly resistant Cretaceous rocks outcropping along the Jama knickpoint reach acts as an inflection point between two subprofiles that show well-fitted logarithmic curves, thereby representing a temporary partitioned equilibrium along the Jama River profile.  相似文献   

Skilful Forecasts of Summer Rainfall in the Yangtze River Basin from November     

Philip E.BETT  Nick DUNSTONE  Nicola GOLDING  Doug SMITH  Chaofan LI 《大气科学进展》2023,(11):2082-2091

Variability in the East Asian summer monsoon(EASM) brings the risk of heavy flooding or drought to the Yangtze River basin, with potentially devastating impacts. Early forecasts of the likelihood of enhanced or reduced monsoon rainfall can enable better management of water and hydropower resources by decision-makers, supporting livelihoods and major economic and population centres across eastern China. This paper demonstrates that the EASM is predictable in a dynamical forecast model from the pr...  相似文献   

The Relationship between Model Biases in East Asian Summer Monsoon Rainfall and Land Evaporation     

Ruth GEEN  Marianne PIETSCHNIG  Shubhi AGRAWAL  Dipanjan DEY  F.Hugo LAMBERT  Geoffrey K.VALLIS 《大气科学进展》2023,(11):2029-2052

The East Asian Summer Monsoon(EASM) provides the majority of annual rainfall to countries in East Asia.Although state-of-the-art models broadly project increased EASM rainfall, the spread of projections is large and simulations of present-day rainfall show significant climatological biases. Systematic evapotranspiration biases occur locally over East Asia, and globally over land, in simulations both with and without a coupled ocean. This study explores the relationship between evapotranspiration...  相似文献