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冈底斯明则-程巴斑岩-夕卡岩型Mo-Cu矿床成矿时代与含矿岩石成因 总被引：2，自引：1，他引：1
冈底斯东南缘克鲁-冲木达矿带以发育渐新世斑岩-夕卡岩型Mo-W-Cu成矿作用而有别于冈底斯中新世斑岩-夕卡岩型Cu-Mo-Au矿带,但是对渐新世成矿岩石类型及成因以及渐新世与中新世斑岩成矿作用存在差异的原因尚不清楚,严重制约了该带矿产资源潜力评价.为此,本文选择矿带内程巴斑岩型Mo矿床及明则夕卡岩型Cu矿床开展了成岩与成矿年代学及含矿岩石成因研究.明则矿区与夕卡岩矿化有关的二长岩的结晶年龄为30.4±0.6Ma,表明夕卡岩矿化时代约30Ma,这与程巴斑岩型Mo矿床矿石中辉钼矿Re-Os同位素分析所揭示的约30Ma矿化时代一致.明则二长岩的SiO2含量为55％ ～57％,K2O含量为2.7％ ～5.0％,属于钾玄岩,具有较高的MgO含量(3.5％～6.9％)、Mg#值(57.6～67.2)以及相容元素含量(Cr =34×10-6 ～379×10-6;Ni为48×10-6～116×10-6).而程巴花岗闪长岩的SiO2含量为65％ ～ 67％,K2O含量为3.2％～4.1％,属于高钾钙碱性岩,具有较低的MgO含量(1.7％～2.1％)、Mg#值(49.5～51.1)以及相容元素含量(Cr =20×10-6～39×10-6;Ni为16×10-6 ～25×10-6).二长岩和花岗闪长岩均显示富集轻稀土元素与大离子亲石元素,亏损高场强元素,具有弱的Eu负异常,但二长岩的REE含量明显高于花岗闪长岩,且具有较低的Sr/Y比值(24 ～49),后者Sr/Y比值为54～68.两种岩石均具有类似的Hf同位素组成,二长岩的εHf(t)值为+2.8～+6.8,花岗闪长岩εHf(t)值为+4.2～ +6.1.综合分析表明,二长岩是受大洋板片流体交代的富集岩石圈地幔部分熔融的产物,而花岗闪长岩是增厚的新生下地壳部分熔融的产物,二者在形成过程中可能发生了幔源镁铁质岩浆与壳源长英质岩浆的混合作用,这种壳幔相互作用导致区域斑岩-夕卡岩型Cu-Mo矿化,但由于该区隆升剥蚀强烈,上部的斑岩型Cu矿体基本被剥蚀而没有保存下来,因此现今表现为斑岩型Mo矿床. 相似文献
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西北太平洋黑潮路径变化与柔鱼CPUE的关系研究 总被引：7，自引：0，他引：7
利用西北太平洋长时间序列SST、黑潮路径、柔鱼渔获量数据,基于GIS技术分析了黑潮路径类型变化和离岸摆动及其对柔鱼CPUE的影响。分析结果表明,1990—2003年,黑潮弯曲发生的月份数占82％,其中整月发生弯曲的月份数占47％,共发生2次大弯曲、2次准弯曲、5次小弯曲。柔鱼年CPUE,在黑潮发生准弯曲年份最高,黑潮发生小弯曲年份较高,黑潮发生大弯曲年份和平直年份较低,黑潮大弯曲发生的强盛年份最低。柔鱼月CPUE高值时段,多是黑潮发生弯曲时段,且主要是C型弯曲。连续3月以上出现月CPUE高值段,黑潮路径模式是C型弯曲和平直路径交替出现。3天CPUE的高值时段,黑潮弯曲型的频次远高于平直型;较高值时段,黑潮弯曲型的频次稍高于平直型;中值时段,黑潮平直型频次稍高于弯曲型;较低值时段,黑潮平直型高于弯曲型;低值时段,黑潮平直型远高于弯曲型。 相似文献
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中国东北漫岗黑土区切沟侵蚀发育特征 总被引：4，自引：0，他引：4
In this study, short-term gully retreat was monitored from the active gullies selected in representative black soil area,
using differential global positioning system (GPS). With the support of geographic information system (GIS), multi-temporal
digital elevation models (DEM) were constructed from the data collected by GPS and used for further analysis. Based on the
analysis of multi-temporal DEM, we discussed the erosion-deposition characteristics within gully and a developing model for
black soil gully area of Northeast China was proposed. The results are: (1) The analysis of the monitored gully data in 2004
indicated that the retreat of gully head reached more than 10 m, gully area extended 170–400 m2, net gully eroded volume 220–320 m3, and gully erosion modulus 2200–4800 t·km−2·a−1. (2) Compared with the mature gully the initial gully grows rapidly, and its erosion parameters are relatively large. The
erosion parameters have not only to do with flow energy, but also with the growth phase. (3) There are significant seasonal
differences in gully erosion parameters. The extension of gully area and width dominates in winter and spring without marked
net erosion while changes mainly occur in gully head and net erosion in rainy season. (4) It is remarkable for freeze-thaw
erosion in the black soil area of NE China. The gully wall of SG2 extended 0.45 m under freeze-thaw effect in 2004, and the
distance of gully head retreated maximally 6.4 m. (5) Due to freeze-thaw action and snowmelt, gully is primarily in the interior
adjustment process in winter and early spring. There are much more depositions compared with that during rainy season, which
can almost happen throughout the gully, while erosion mostly occurs near head, esp. for gullies having a relatively long history
of development. On the other hand, the process of energy exchange with exterior dominates in rainy season. It is considered
that this cyclic process is an important mechanism for gully growth in high latitude or/and high attitude regions.
Foundation: Key Project for National Natural Science Foundation of China, No.40235056; The Ph.D. Programs Foundation of Ministry of Education
of China, No.20030027015; China Postdoctoral Science Foundation, No.20070410482; Doctoral Foundation of University of Jinan,
No.B0620; National Natural Science Foundation of China, No.40672158; Key Subject Foundation Supported by Shandong Province
Author: Hu Gang (1976–), Ph.D and Associate Professor, specialized in soil erosion, environmental evolution and regional planning. 相似文献
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西北太平洋柔鱼中心渔场分布模式 总被引：10，自引：1，他引：9
本文利用ArcGIS对西北太平洋SST和柔鱼渔捞统计时间序列数据进行了处理分析 ,研究了西北太平洋柔鱼中心渔场分布模式。该海域柔鱼中心渔场有三类 :舌型渔场、枝叉型渔场、涡流型渔场。涡流型渔场出现次数最高、渔获总产量最高、CPUE平均值最高 ,表层水温为 10～ 18℃。舌型渔场出现次数第二、渔获总产量第二、CPUE平均值最低 ,表层水温为 15～2 1℃。枝叉型渔场出现次数最少、渔获总产量最低、CPUE平均值第二 ,表层水温为 17～2 4℃。 8月枝叉型渔场为主 ,9月舌型渔场为主 ,10月舌型渔场和涡流型渔场为主 ,11月涡流型渔场为主。 相似文献
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