松树沟元古宙蛇绿岩Nd、Sr、Pb同位素地球化学特征

松树沟蛇绿岩中镁铁质岩的Sm-Nd全岩等时年龄为1030±46Ma,∈Nd(t)=+5.7,模式年龄在1422-1271Ma之间,矿物的内部等时年龄为983±140Ma。全岩等时年龄为其形成上限,矿物内部等时年龄为其变质年龄,说明该蛇绿岩形成于中元古代中、晚期。镁铁质岩的∈Nd(t)在+4.2-+6.9之间,是DMM与EMI两个地幔端元的混合产物;206Pb/204Pb在18.06-18.66之间,207Pb/204Pb和208Pb/204Pb值较高,分别在15.55-15.60和37.59-38.38之间,207Pb/204Pb和208Pb/204Pb对206Pb/204Pb的关系表明,岩浆源于具DUPAL异常的源区,(207Pb/204Pb)i相对(208Pb/204Pb)i更偏离NHRL可能是变质流体作用的反映。∈Sr(t)值较高且变化大,可与蛇绿岩类比,87Sr/86Sr比值变化大,可能与海水蚀变作用有关。据此推测,松树沟蛇绿岩代表洋壳残片。     

塔里木盆地哈拉哈塘地区奥陶系一间房组岩溶储集层地震识别与控制因素*

哈拉哈塘地区位于塔里木盆地北部隆起轮南低凸起奥陶系潜山背斜西翼上,其中奥陶系一间房组碳酸盐岩岩溶储集层具有成因复杂、非均质性强和识别困难等特点。以该地区现有钻井资料、地震解释成果为基础,在现代岩溶研究成果的指导下,利用分时窗提取、断裂属性(Fault Fracture Attribute,FFA)裂缝预测等特色技术,详细刻画了一间房组孔洞、裂缝型储集层空间分布特征。利用地层CT扫描古河道识别、残厚法古地形恢复、基于优化算法的构造识别体断裂精细刻画等特色技术开展了岩溶储集层控制因素分析,指出古地形较高、水系发达、小断裂发育等是一间房组岩溶储集层发育的有利控制因素。面对现有碳酸盐岩岩溶储集层勘探难题,以现代岩溶理论为指导,钻井-地震结合,综合利用多种地震预测技术是开展研究区碳酸盐岩岩溶储集层识别和控制因素分析的重要手段。     

构造煤与原生结构煤的显微傅立叶红外光谱特征对比研究

通过对平顶山、郑州和南票三大矿区石炭二叠纪含煤岩系中高煤级烟煤和无烟煤的显微傅立叶红外光谱分析，探讨了原生结构煤与构造煤的有机大分子结构演化特征及其影响因素。结果表明，构造应力有利于煤中氢发生化学环境转移，使脂肪烃含量相对减少、稳定的芳香烃含量相对增加，促进煤大分子结构缩合度和有序度增加。     

The broad band spectral index of TeV blazars detected by Fermi LAT

Using γ-ray data detected by Fermi Large Area Telescope (LAT) and multi-wave band data for 35 TeV blazars sample, we have studied the possible correlations between different broad band spectral indices ( $\alpha_{\rm r.ir}$ , $\alpha_{\rm{r.o}}$ , $\alpha_{\rm r.x}$ , $\alpha_{\rm r.\gamma}$ , $\alpha_{\rm{ir.o}}$ , $\alpha_{\rm ir.x}$ , $\alpha_{\rm ir.\gamma}$ , $\alpha_{\rm o.x}$ , $\alpha_{\rm o.\gamma}$ , $\alpha_{\rm r.x}$ , $\alpha_{\rm x.\gamma}$ ) in all states (average/high/low). Our results are as follows: (1) For our TeV blazars sample, the strong positive correlations were found between $\alpha_{\rm r.ir}$ and $\alpha_{\rm{r.o}}$ , between $\alpha_{\rm r.ir}$ and $\alpha_{\rm r.x}$ , between $\alpha_{\rm r.ir}$ and $\alpha_{\rm r.\gamma}$ in all states (average/high/low); (2) For our TeV blazars sample, the strong anti-correlations were found between $\alpha_{\rm r.ir}$ and $\alpha_{\rm x.\gamma}$ , between $\alpha_{\rm{r.o}}$ and $\alpha_{\rm ir.\gamma}$ , between $\alpha_{\rm{r.o}}$ and $\alpha_{\rm o.\gamma}$ , between $\alpha_{\rm{r.o}}$ and $\alpha_{\rm x.\gamma}$ , between $\alpha_{\mathrm{ir.o}}$ and $\alpha_{\rm o.\gamma}$ , between $\alpha_{\rm r.x}$ and $\alpha_{\rm x.\gamma}$ , between $\alpha_{\rm ir.x}$ and $\alpha_{\rm x.\gamma}$ in all states (average/high/low). The results suggest that the synchrotron self-Compton radiation (SSC) is the main mechanism of high energy γ-ray emission and the inverse Compton scattering of circum-nuclear dust is likely to be a important complementary mechanism for TeV blazars. Our results also show that the possible correlations vary from state to state in the same pair of indices, Which suggest that there may exist differences in the emitting process and in the location of the emitting region for different states.     

有关地理纬度和地心纬度的换算问题

本文简要地从地理纬度α与地心纬度φ的基本换算公式导出它的近似公式,并用最新的地球扁率值 e 给出基本公式中和近似公式中的换算系数β和γ,进而给出α—φ的换算新表。新旧两表最大可差5角秒(对应地面距离达150米)。这在一些对纬度换算精度要求较高的地学问题中是不容忽视的。本文最后还对近似公式做了简要讨论。     

湖北宜昌石板溪金矿区断层空间结构及其控矿规律研究

断层空间结构包括变形结构和几何结构两部分。本文在解析石板溪金矿区主要断层变形结构和几何结构的基础上，探讨了其空间结构模式和控矿规律。     

Abundances of Jupiter's trace hydrocarbons from Voyager and Cassini

The flybys of Jupiter by the Voyager spacecraft in 1979, and over two decades later by Cassini in 2000, have provided us with unique datasets from two different epochs, allowing the investigation of seasonal change in the atmosphere. In this paper we model zonal averages of thermal infrared spectra from the two instruments, Voyager 1 IRIS and Cassini CIRS, to retrieve the vertical and meridional profiles of temperature, and the abundances of the two minor hydrocarbons, acetylene (C₂H₂) and ethane (C₂H₆). The spatial variation of these gases is controlled by both chemistry and dynamics, and therefore their observed distribution gives us an insight into both processes. We find that the two gases paint quite different pictures of seasonal change. Whilst the 2-D cross-section of C₂H₆ abundance is slightly increased and more symmetric in 2000 (northern summer solstice) compared to 1979 (northern fall equinox), the major trend of equator to pole increase remains. For C₂H₂ on the other hand, the Voyager epoch exhibits almost no latitudinal variation, whilst the Cassini era shows a marked decrease polewards in both hemispheres. At the present time, these experimental findings are in advance of interpretation, as there are no published models of 2-D Jovian seasonal chemical variation available for comparison.     

Improved understanding of petroleum migration history in the Hongche fault zone,northwestern Junggar Basin (northwest China): Constrained by vein-calcite fluid inclusions and trace elements

Calcite veins and cements occur widely in Carboniferous and Permian reservoirs of the Hongche fault zone, northwestern Junggar Basin in northwest China. The calcites were investigated by fluid inclusion and trace-element analyses, providing an improved understanding of the petroleum migration history. It is indicated that the Hongche fault behaved as a migration pathway before the Early Cretaceous, allowing two oil charges to migrate into the hanging-wall, fault-core and footwall reservoirs across the fault. Since the Late Cretaceous, the Hongche fault has been sealed. As a consequence, meteoric water flowed down only into the hanging-wall and fault-core reservoirs. The meteoric-water incursion is likely an important cause for degradation of reservoir oils. In contrast, the footwall reservoirs received gas charge (the third hydrocarbon event) following the Late Cretaceous. This helps explain the distribution of petroleum across the fault. This study provides an example of how a fault may evolve as pathway and seal over time, and how reservoir diagenetic minerals can provide clues to complex petroleum migration histories.     

EVIDENCE OF NEOTECTONIC IMPACT ON A LARGE SEDIMENTARY BASIN BETWEEN TIBETAN PLATEAU AND GOBI ALTAY,NW CHINA

The Ejina(Gaxun Nur)Basin­enclosed by the Tibetan Plateau in the south and the Gobi Altay in the north has continuously evolved as a strong continental endorheic depositional environment. Medium scale geomorphological mapping by Landsat­ and Corona­Images as well as SRTM­topographic data,combined with field­surveys and geophysical investigation provides evidence for tectonic impact on sedimentary processes during the Late Quaternary.
Analyses of SRTM­Data and Landsat­Images reveal a system of up to 20m high inverted channels developed on the inactive eastern part of the large Hei river drainage delta south of the ancient lake Juyanze. The complex evolution of these landforms requires a relative lowering of the lake basin at least two times since the last 40ka. A 26m high cliff section of gravel­covered lake sediments within the Juyanze paleolake indicates a strong subsidence of the lake bottom of 10m/1000yrs since 18kaB.P.
North of Ejina river oasis a distinct north­south striking scarp up to 13m high constitutes the eastern margin of the Gaxun Nur. Palaeodrainage channels derived from the Gobi Altay. They display a sinistral offset of some decametres along a set of WE­trending faults. The rhombic shape of the modern dry Gaxun Nur,fossil cliffs,well preserved beach ridges along the margins of the palaeolake system as well as gravel covered topsets of lacustrine sediments indicate local displacements of morphological features. The displacements of lake sediments at the southern margin of the modern Gaxun Nur Basin imply a subsidence of at least 0.81m/1000 yrs since 25kaB.P.as a result of a pull­apart development due to the left stepping faults in a sinistral system.