胶西北金矿集区成矿作用发生的地质背景

通过矿集区赋存的地质背景 ,包括区域重大地质事件、壳幔结构、深断裂及浅层断裂系的导流性、区域流体活动、地层建造及岩浆侵入事件等研究 ,建立了矿集区形成与演化框架 ,并提出了形成的必备因素。成矿诸因素间彼此关联、耦合为大型矿集区的形成提供了必备而优越的条件。地质演化历史中构造体制转换事件是大规模成矿作用发生的基础 ,其引起的区域壳幔物质交换、岩浆活动等系列事件及耦合作用为区域成矿作用提供了充足成矿物质、良好导流网络、丰富成矿流体、持续成矿能量等必备条件 ,最终导致矿集区的形成。     

中国大陆构造中的西秦岭-松潘大陆构造结

位于中国大陆中部的西秦岭—松潘大陆构造结属于地壳尺度上的巨型构造。该巨型构造是在中国大陆完成其主体拼合过程中 ,在特提斯阿尔卑斯—喜马拉雅、太平洋和古亚洲及其后的环西伯利亚弧形构造三大构造动力学体系共同作用下 ,由构成中国大陆的主要造山带及地块交接汇聚而成 ,成为东西向的中国大陆中央造山系、近南北向的川滇—贺兰构造带和中新生代以来形成的青藏高原之间交接转换的关键构造域。在先期构造基础上 ,构造结形成具有东、西和北三个重要边界以及内部东北、东南、西南和南端等多个具体构造结点。其内部主干构造勉略—阿尼玛卿构造带又将其划作西秦岭和松潘地块南北两部分。西秦岭—松潘构造结主要形成于中国大陆印支主拼合期 ,并叠加印支期后陆内构造。构造结内组成与结构复杂 ,构造样式繁多 ,包含有丰富的大陆地质信息 ,实属研究中国大陆地质与大陆动力学不可多得的天然实验室     

Nearshore wave environments around a sandy cay on a platform reef,Torres Strait,Australia

Waves are the primary factor affecting reef-island morphology. This study examines spatial and temporal variations of wave characteristics in the nearshore around Warraber Island, a sandy cay on a platform reef in Torres Strait Australia, based on field measurements during the predominant southeasterly wind season. Water pressure was recorded simultaneously, and transformed to water surface wave spectra, at a location close to the reef edge and across the nearshore at different locations around the island. Wave environments off the reef were estimated based on wave characteristics measured at the reef-edge location and found to be primarily dominated by sea. Low and high wave-energy events were identified, based on wave energy level at the reef-edge location.     

移动荷载作用下层状饱和土的动力响应

根据Biot波动理论,采用传递、反射矩阵（TRM）方法研究了移动荷载作用下层状饱和土动力响应问题。由快速Fourier逆变换法（IFFT）得到层状土地基位移、应力及孔压在时间-空间域内的数值解。计算结果与已有文献结果相吻合,验证了算法的正确性。通过算例分析表明：移动荷载作用下含有软弱夹层的层状土体比均质土具有更显著的动力响应,同时会引起土体孔隙水压升高、土体波动性增强;硬夹层时情况则相反。     

电偶源瞬变电磁测深研究(五)--实测感应电压转换成垂直磁场

阐述了电偶源瞬变电磁测深感应电压Ｖｚ（ｔ）转换为垂直磁场Ｈｚ（ｔ）的方法,以便计算全区视电阻率,进行定性与定量解释。     

倾斜台阶重力异常灰色反演

迄今为止,想直接利用某一种重务异常曲线求解台阶是类隐 伏地质体的物性和几何参数是十分困难的,一般只能从异常曲线特征上作定性分析,详细分析了倾斜台阶△ｇ重力异常的理论公式及其特下点列的性质,提出了倾斜台阶的重力异常、规范特征点春序列以及差比变换等新概念,建立了直接利用△ｇ曲线反演倾斜台阶全部未特点及其序以及差比变换街等概念,建立了直接利用△ｇ曲线反演中队全部未知参数的一种新解法－规范特征点序列灰关联     

Automatic searching of control point in NOAA AVHRR image

This paper discusses the approaches for automatical searching of control points in the NOAA AVHRR image on the basis of data rearrangement in the form of latitude and longitude grid. The vegetation index transformation and multi-level matching strategies have been proven effective and successful as the experiments show while the control point database is established.     

椭球的倾斜像面空间透视投影正反解变换

利用矢量方法推出椭球的倾斜像面空间透视投影正解公式, 计算出此正解公式与球体的相应正解公式之间的误差, 并且利用矢量方法导出其相应反解公式。     

Fast transform from geocentric to geodetic coordinates

 A new iterative procedure to transform geocentric rectangular coordinates to geodetic coordinates is derived. The procedure solves a modification of Borkowski's quartic equation by the Newton method from a set of stable starters. The new method runs a little faster than the single application of Bowring's formula, which has been known as the most efficient procedure. The new method is sufficiently precise because the resulting relative error is less than 10⁻¹⁵, and this method is stable in the sense that the iteration converges for all coordinates including the near-geocenter region where Bowring's iterative method diverges and the near-polar axis region where Borkowski's non-iterative method suffers a loss of precision. Received: 13 November 1998 / Accepted: 27 August 1999     

On the adjustment of combined GPS/levelling/geoid networks

A detailed treatment of adjustment problems in combined global positioning system (GPS)/levelling/geoid networks is given. The two main types of `unknowns' in this kind of multi-data 1D networks are usually the gravimetric geoid accuracy and a 2D spatial field that describes all the datum/systematic distortions among the available height data sets. An accurate knowledge of the latter becomes especially important when we consider employing GPS techniques for levelling purposes with respect to a local vertical datum. Two modelling alternatives for the correction field are presented, namely a pure deterministic parametric model, and a hybrid deterministic and stochastic model. The concept of variance component estimation is also proposed as an important statistical tool for assessing the actual gravimetric geoid noise level and/or testing a priori determined geoid error models. Finally, conclusions are drawn and recommendations for further study are suggested. Received: 9 September 1998 / Accepted: 8 June 1999