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1.
胶东内生金矿成矿期次和成矿时代的讨论 总被引：4，自引：0，他引：4
胶东地区内生金矿的成矿溶液是深溶岩浆连续分异演化而成.成岩成矿作用产生于同一个地质时代,并可分为包括岩浆岩体、脉岩、矿床及其诸成矿阶段在内的早晚两期成矿系列.早期的内生金矿为主生金矿期.晚期为共生—伴生金矿期.早期成矿系列生成时代于156～136Ma之间,晚期为124～100Ma. 相似文献
2.
The occurrence and development of riparian forests, which were mainly dominated by mesophytes species related closely with
surface water. Since there was no water discharged to the lower reaches of Tarim River in the past three decade years, the
riparian forests degrade severely. The groundwater table, the saline content of the groundwater, as well as the content of
free proline, soluble sugars, plant endogenous hormones (abscisic acid (ABA), and cytokinins (CTK)) of the leaves and relative
rates of sap flow of the Populus euphratica Oliv. (arbor species), Tamarix ramosissima Ldb. (bush species), and Apocynum venetum L. (herb species) were monitored and analyzed at the lower reaches of the Tarim River in the study area where five positions
on a transect were fixed at 100 m intervals along a sampling direction from riverbank to the sand dunes before and after water
release. The physiological responses and acclimation strategies of three species to variations in water and salinity stress
were discussed. It was found that A. venetum population recovered to groundwater table ranging from −1.73 to −3.56 m, and when exposed to saline content of the groundwater
ranging from 36.59 to 93.48 m mol/L; P. euphratica appeared to be more sensitive to the elevation of groundwater table than the A. venetum and T. ramosissima at groundwater table ranging from −5.08 to −5.80 m, and when exposed to saline content of the groundwater ranging from 42.17
to 49.55 m mol/L. T. ramosissima tended to be the best candidate species for reclamation in this hyper-arid area because it responded to groundwater table
ranging from −1.73 to −7.05 m, and when exposed to saline content of the groundwater ranging from 36.59 to 93.48 m mol/L.
These results explained the distribution patterns of desert vegetation in the lower reaches of the Tarim River. Understanding
the relationships among ecological factors variables, physiological response and acclimation strategies of plant individuals
could provide guidance to sustainable management, reclamation and development of this and similar regions. 相似文献
3.
大兴安岭地区内生铜矿床的成因类型、成矿时代与成矿动力学背景 总被引：11，自引：4，他引：7
大兴安岭地区位于兴蒙造山带的东段,构造、岩浆活动强烈,蕴藏着丰富的内生有色金属、贵金属矿产资源。本文通过对该区内生铜矿床的地质特征、成因类型和年代学研究,初步将区内内生铜矿床划分为斑岩型、浅成热液高硫化型(铜银、铜锡)和接触交代型三种成因类型,除铜锡矿床外,它们的成矿作用均与高钾钙碱系列I型花岗质岩浆密切相关;其中斑岩型和浅成热液高硫化型(铜、银)的成矿分别发生在485Ma、180~170Ma和170~160Ma;而浅成热液高硫化型(铜锡)矿床与A型花岗质岩浆相关,成矿在150~135Ma之间;接触交代型与它们相伴生,主要发生在180~160Ma和150~135Ma。其成矿动力学背景分别与早古生代兴安地块与松嫩地块的拼合碰撞造山、中侏罗世的西伯利亚板块和华北板块的陆缘增生带碰撞缝合造山与早白垩世碰撞造山后的地壳伸展减薄作用过程相适应,矿床在不同阶段的造山挤压与伸展转换或造山期后的伸展阶段就位,这项研究为深入研究该区内生多金属成矿规律提供了科学依据。 相似文献
4.
内源酶是三疣梭子蟹(Portunus trituberculatus)体内重要的酶,往往会导致梭子蟹死后肌肉组织迅速软化,严重影响了蟹肉的贮藏品质。为了探明该酶的基本特性,本试验从三疣梭子蟹肝胰腺中提取了粗酶,优化了提取方法,并对其部分酶学性质进行初步研究。结果表明:三疣梭子蟹肝胰腺内源酶最佳浸提时间段为4～12 h,酶比活显著高于0～4 h和12～14 h;以酪蛋白为水解底物,内源酶作用最适温度为65℃、最适p H范围为7.0～8.0;丝氨酸蛋白酶特异性抑制剂,包括大豆胰蛋白酶抑制剂(SBTI)和苯甲基磺酰氟(PMSF),对内源酶活力的相对抑制率分别为100%、70.46%±6.27%,显著高于其他抑制剂的相对抑制率,推测丝氨酸蛋白酶为主要内源酶;在硫酸铵分级沉淀中,分别以酪蛋白和Boc-Phe-Ser-Arg-MCA为底物,前者最适盐析浓度为0～70%,后者为30%～70%,酶比活显著高于其他盐浓度;当硫酸铵浓度为40%～60%时,盐析蛋白质含量、粗酶酶活和丝氨酸蛋白酶活均显著高于其他盐浓度。 相似文献
5.
Laurent Viguier Leonardo Barreto Alain Haurie Socrates Kypreos Peter Rafaj 《Climatic change》2006,79(1-2):121-141
In this two-part paper we evaluate the effect of “endogenizing” technological learning and strategic behavior of agents in economic models used to assess climate change policies. In the first part we show the potential impact of R&D policies or demonstration and deployment (D&D) programs in the context of stringent stabilization scenarios. In the second part we show how game-theoretic methods can be implemented in climate change economic models to take into account three types of strategic interactions: (i) the market power of the countries benefiting from very low abatement costs on international markets for CO2 emissions, (ii) the strategic behavior of governments in the domestic allocation of CO2 emissions quotas, and (iii) the non-cooperative behavior of countries and regions in the burden sharing of CO2 concentration stabilization. The two topics of endogenous learning and game-theoretic approach to economic modeling are two manifestations of the need to take into account the strategic behavior of agents in the evaluation of climate change policies. In the first case an R&D policy or a demonstration and deployment (D&D) program are put in place in order to attain a cost reduction through the learning effect; in the second case the agents (countries) reply optimally to the actions decided by the other agents by exploiting their strategic advantages. Simulations based on integrated assessment models illustrate the approaches. These studies have been conducted under the Swiss NCCR-Climate program. 相似文献
6.
Can sandy beach molluscs show an endogenously controlled circatidal migrating behaviour? Hints from a swash rig experiment 总被引：1，自引：0，他引：1
Many macrofaunal species inhabiting exposed sandy beaches are dependent on the swash for their nutrition and migration and are highly adapted to the harsh physical conditions of the swash. The most important physical factors that determine the distribution and behaviour of swash related fauna, next to the swash itself, are sediment grain size and beach slope. Crucial swash parameters are swash period and swash velocity. Studying the influence of these factors on the animals in the field is often very difficult and it is almost impossible to identify which factor causes what effect. Crucial knowledge about the direct role of the swash itself is lacking. Therefore, a device that generates swash waves on an artificial beach under laboratory conditions was designed: the swash rig. In the swash rig, full and independent control on sediment grain size, beach slope, swash velocity and swash period is present. This will allow us to do a variety of experiments on the influence of each of these factors, independently or combined, on swash fauna. In one such experiment, Olivella semistriata – a dominant surfing gastropod on Ecuadorian sandy beaches – was placed in the swash rig during rising and falling tide and subjected – under constant conditions – to an equal wave regime. During falling tide, and in absence of any tidal cue, almost all specimens moved downshore, as they would in the field; hardly any specimens moved upshore. During upcoming tide, however, there was noticeable upward migration in the swash rig, and half of the runs showed a net upward migration. Contrary to the common understanding that the behaviour of sandy beach molluscs is entirely environmentally driven, this experiment hints at the presence of an endogenous circatidal clock, which is used to direct the tidal migration of the species. 相似文献
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On King George Island during latest Oligocene/earliest Miocene time, submarine eruptions resulted in the emplacement of a
small (ca. 500 m estimated original diameter) basalt lava dome at Low Head. The dome contains a central mass of columnar rock
enveloped by fractured basalt and basalt breccia. The breccia is crystalline and is a joint-block deposit (lithic orthobreccia)
interpreted as an unusually thick dome carapace breccia cogenetic with the columnar rock. It was formed in situ by a combination
of intense dilation, fracturing and shattering caused by natural hydrofracturing during initial dome effusion and subsequent
endogenous emplacement of further basalt melt, now preserved as the columnar rock. Muddy matrix with dispersed hyaloclastite
and microfossils fills fractures and diffuse patches in part of the fractured basalt and breccia lithofacies. The sparse glass-rich
clasts formed by cooling-contraction granulation during interaction between chilled basalt crust and surrounding water. Together
with muddy sediment, they were injected into the dome by hydrofracturing, local steam fluidisation and likely explosive bulk
interaction. The basalt lava was highly crystallised and degassed prior to extrusion. Together with a low effusion temperature
and rapid convective heat loss in a submarine setting, these properties significantly affected the magma rheology (increased
the viscosity and shear strength) and influenced the final dome-like form of the extrusion. Conversely, high heat retention
was favoured by the degassed state of the magma (minimal undercooling), a thick breccia carapace and viscous shear heating,
which helped to sustain magmatic (eruption) temperatures and enhanced the mobility of the flow.
Received: 1 August 1996 / Accepted: 15 September 1997 相似文献
10.
依据大地电磁测深所发现的上地幔高导层顶面深度可以给出大陆岩石圈-软流圈界面(LAB)的空间发育特征,为认识岩石圈结构及壳幔相互作用等提供重要信息.本文在1996年编制的中国大陆上地幔高导层顶面深度图的基础上,补充了1995—2010年大地电磁测深结果和大地热流数据,以1°×1°网度编制了新的中国大陆上地幔高导层顶面深度图.我国上地幔高导层顶面深度变化很大,具有南北分带,东西分块的特征,呈东浅、西深、北浅、南深的格局,从最浅的50~60km到最深的230km,平均深度为100~120km.据上地幔高导层顶面分布形态,全国共可划分出27个隆起区.通过与中国已知内生金属矿产和油气田的分布对比,发现我国大陆80%以上中生代内生金属矿床分布在上地幔高导层隆起带或其梯度带上方.中国大陆东部含油气盆地主体对应上地幔隆起区,油气田多位于隆起区上方或其边部的过渡带上;西部主体位于幔坳区,主要油气田对应盆地中心的幔坳向周边幔隆过渡的梯度带上;中部表现为仅盆地腹地对应幔坳,盆地周边对应规模较大的上地幔隆起带,主要油气田位于隆起带.总的来看内生金属矿床一般分布在上地幔隆起区靠近造山带一侧,而油气田一般分布在上地幔隆起区靠近盆地一侧.软流圈的不断上隆,造成岩石圈减薄、拉张,张性断裂的出现成为地球深部物质和热量向地壳上部运移的有利通道,为内生金属矿产的形成提供了成矿物质和能量保障,也为含油气盆地带来了生烃催化剂、热能和无机成因的石油与天然气.地球深部超临界流体的存在对上地幔高导层的形成、成矿物质运移可能发挥了重要作用. 相似文献