海底天然气渗漏系统水合物成藏动力学及其资源评价方法

根据海底天然气渗漏系统沉淀水合物的动力学模型,计算了海底渗漏系统中渗漏天然气沉淀为水合物的比例。如果BushHill渗漏系统海底水合物或喷溢天然气的化学组成是渗漏系统气源天然气通过沉淀水合物转变而成,则需要约3. 3% ~21. 7% (平均12. 9% )的渗漏天然气在海底沉淀为水合物。结合渗漏系统的活动时间(1万年)和天然气流量(800t/a),沉淀在墨西哥湾GC185区BushHill渗漏系统中的水合物天然气资源为0. 37×109 ~2. 43×109 m3,平均为1. 45×109 m3,与体积和含量评价方法获得的结果基本一致。     

Source contributions to Devonian granite magmatism near the Laurentian border, New Hampshire and Western Maine, USA

Radiogenic isotope data (initial Nd, Pb) and elemental concentrations for the Mooselookmeguntic igneous complex, a suite of mainly granitic intrusions in New Hampshire and western Maine, are used to evaluate petrogenesis and crustal variations across a mid-Paleozoic suture zone. The complex comprises an areally subordinate monzodiorite suite [377±2 Ma; ε_Nd (at 370 Ma)=−2.7 to −0.7; initial ²⁰⁷Pb/²⁰⁴Pb=15.56–15.58] and an areally dominant granite [370±2 Ma; ε_Nd (at 370 Ma)=−7.0 to −0.6; initial ²⁰⁷Pb/²⁰⁴Pb=15.55–15.63]. The granite contains meter-scale enclaves of monzodiorite, petrographically similar to but older than that of the rest of the complex [389±2 Ma; ε_Nd (at 370 Ma)=−2.6 to +0.3; initial ²⁰⁷Pb/²⁰⁴Pb 15.58, with one exception]. Other granite complexes in western Maine and New Hampshire are 30 Ma older than the Mooselookmeguntic igneous complex granite, but possess similar isotopic signatures.

Derivation of the monzodioritic rocks of the Mooselookmeguntic igneous complex most likely occurred by melting of Bronson Hill belt crust of mafic to intermediate composition. The Mooselookmeguntic igneous complex granites show limited correlation of isotopic variations with elemental concentrations, precluding any significant presence of mafic source components. Given overlap of initial Nd and Pb isotopic compositions with data for Central Maine belt metasedimentary rocks, the isotopic heterogeneity of the granites may have been produced by melting of rocks in this crustal package or through a mixture of metasedimentary rocks with magmas derived from Bronson Hill belt crust.

New data from other granites in western Maine include Pb isotope data for the Phillips pluton, which permit a previous interpretation that leucogranites were derived from melting heterogeneous metasedimentary rocks of the Central Maine belt, but suggest that granodiorites were extracted from sources more similar to Bronson Hill belt crust. Data for the Redington pluton are best satisfied by generation from sources in either the Bronson Hill belt or Laurentian basement. Based on these data, we infer that Bronson Hill belt crust was more extensive beneath the Central Maine belt than previously recognized and that mafic melts from the mantle were not important to genesis of Devonian granite magma.     

济阳坳陷古桩西断层的发现及其对桩西潜山 形成的影响

北西向断层是济阳坳陷成生较早的重要的控盆断裂,并对后期构造的产生具有重要的影响。本文在济阳坳陷桩西潜山地区三维地震资料精细解译的基础上,识别出了一条北西向断层,将其命名为古桩西断层,并分析了该断层的叠加改造过程和改造方式,以及对桩西潜山形成的影响。研究结果表明：古桩西断层经历了印支期挤压逆冲、燕山期中期负反转,燕山末期正反转和喜马拉雅期再次负反转,最终被分割成5条独立活动的断层;古桩西断层的叠加改造方式有直接反转、通过应变硬化带反转和被断层错段3种方式;古桩西断层的长期活动控制着北西向桩西潜山的形成以及次一级近南北向雁列状潜山的产生。     

商圈功能多样性对其活力的影响研究

探究功能多样性如何影响商圈活力,可为城市用地功能结构优化调整和商圈功能改造提供理论支撑,进而促进城市混合功能有序开发、提升城市活力.已有关于功能多样性与活力的研究,大多集中在城市、街道活力等方面,对于商圈活力研究很少涉及,且大多利用单一的熵指数反映功能多样性.在利用夜光数据对活力的研究中,大多选取城市或更大区域尺度作为...     

浅谈2.5D磁法反演估算铁矿资源量的多解性

2.5D磁法反演估算铁矿资源量,关键是在垂直磁异常走向上求拟合模型的截面积。该文利用一种常见模型拟合4种实测磁场,发现铁矿截面积与埋深和磁性大小有一定的规律:磁化强度一定时,截面积与埋深呈线性正相关;埋深一定时,截面积与磁化强度呈近似指数形式的反相关。固定深部或外围磁性体参数,单独考虑浅部或中间铁矿模型时也有这种规律。在无钻孔资料及磁性资料不清楚时,磁化强度100 000×10-3~150 000×10-3A/m为估算铁矿资源量的最佳磁参数。因磁法反演的多解性,此类方法适用于钻孔验证前的资源量估计。