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Początki królestwa zwierząt – preludium eksplozji kambryjskiej 动物王国的开端——寒武纪大爆发的前奏
Q4 Earth and Planetary Sciences Pub Date : 2022-09-14 DOI: 10.7306/2022.19
A. Majchrzyk, A. Żylińska
of life on Earth when diverse animal phyla burst into existence almost from nowhere. However, despite this sudden appearance, the fossil record and evolutionary history of animals goes much deeper in time into the Neoproterozoic. This contribution reviews the earliest known faunas, their diversity and ecological complexity. Moreover, specimens of Ediacaran biota from the Polish museum collections are briefly presented.
各种各样的动物门类几乎从任何地方突然出现。然而,尽管这种突然出现,动物的化石记录和进化历史可以追溯到新元古代。这篇文章回顾了已知最早的动物群,它们的多样性和生态复杂性。此外,还简要介绍了波兰博物馆收藏的埃迪卡拉动物群标本。
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引用次数: 0
Ściśliwość wybranych gruntów drobnoziarnistych z centralnej Polski w warunkach stałego przyrostu obciążenia 恒定荷载增加条件下波兰中部选定细粒土的紧密性
Q4 Earth and Planetary Sciences Pub Date : 2022-08-03 DOI: 10.7306/2022.16
P. Stajszczak
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引用次数: 0
Chondryt węglisty NWA 4446 碳化球粒陨石NWA 4446
Q4 Earth and Planetary Sciences Pub Date : 2022-08-03 DOI: 10.7306/2022.17
T. Przylibski, Konrad Blutstein, K. Łuszczek, Joanna Gruchot
4446. Prz. 513–526; A b s t r a c t. The authors carried out petrographic, mineralogical, and chemical analyses (bulk chemical composition and microanalyses of mineral chemical composition) of NWA 4446 carbonaceous chondrite. NWA 4446 chondrite is classified as CV3, S2, W2. This meteorite is a rock fragment most likely from one of the C-type asteroids orbiting the Sun in the outer part of the asteroid belt. It represents the matter formed at the earliest stages of the formation of extrasolar bodies in the solar system. As a result of the research, the authors documented a wider range of variation in the chemical composition of olivine crystals (Fa: 0.67–46.57 mol%) in the matrix and chondrules, and a much narrower range of variation in the chemical composition of pyroxene crystals (Fs: 0.90–3.35 mol%) against the data used for the classification of the meteorite. The characteristics of the chondrules, ranging in size from 0.5 to more than 1 mm, allowed concluding that they constitute about 60% of the meteorite’s volume, in which they form many structural and mineral varieties PO, POP, BO, PP and RP chondrules were observed. The remaining 40% of the chondrite volume is a matrix consisting of small crystals of pyroxenes, olivines, glass, as well as opaque minerals: sulphides, FeNi alloy, native copper and gold grains, carbonaceous substance, and compact CAIs. The mineral and chemical composition of CAIs shows that their dominant mineral is melilite, accompanied by diopside and spinel. The chemical composition of spinel and diopside is very similar to their total chemical formulas, while the composition of melilite shows a significant sodium deficiency. Among the opaque minerals, one phase of the FeNi dominates – awaruite (Ni 3 Fe), and sulphides are represented by troilite (FeS) and mackinawite ((Fe,Ni) 9 S 8 ). Moreover, grains of native copper with an admixture of gold and grains of native gold with an admixture of platinum, nickel and copper with a size of several µm were identified. Taking into account the admixtures contained in the above-mentioned opaque minerals (mainly Co and Cu), the parent rock of the carbonaceous chondrite NWA 4446 can be considered to have been mineralized with Fe, Ni, Co and Cu ore minerals with the content of Au and Pt. This means that, we can expect deposits of native forms of the above-mentioned metals and sulphides on the parent bodies of carbonaceous chondrites of the CV group – C-type asteroids.
4446. Prz。513 - 526;作者对NWA 4446碳质球粒陨石进行了岩石学、矿物学和化学分析(整体化学成分和矿物化学成分的微观分析)。NWA 4446球粒陨石分为CV3、S2、W2。这颗陨石是一块岩石碎片,很可能来自小行星带外层绕太阳运行的c型小行星。它代表了太阳系外天体形成的最早阶段形成的物质。作为研究的结果,作者记录了基质和球粒中橄榄石晶体(Fa: 0.67-46.57 mol%)化学成分的变化范围更大,而辉石晶体(Fs: 0.90-3.35 mol%)化学成分的变化范围要小得多,这与用于陨石分类的数据相对照。这些陨石球粒的大小从0.5毫米到1毫米以上不等,它们的特征使得它们占陨石体积的60%左右,其中它们形成了许多结构和矿物品种PO, POP, BO, PP和RP球粒。其余40%的球粒陨石体积是由辉石、橄榄石、玻璃的小晶体以及不透明矿物组成的基质:硫化物、FeNi合金、天然铜和金颗粒、碳质物质和致密的cai。cai的矿物和化学组成表明,其主要矿物为千英石,伴生有透辉石和尖晶石。尖晶石和透辉石的化学组成与其总化学式非常相似,而千英石的化学组成则表现出明显的缺钠。在不透明矿物中,辉钼矿(ni3fe)占主导地位,硫化物以黄铁矿(FeS)和镁铁((Fe,Ni) 9s8)为代表。此外,还发现了含有金的天然铜颗粒和含有铂、镍和铜的天然金颗粒,其尺寸为几µm。考虑到上述不透明矿物(主要是Co和Cu)中所含的掺合物,NWA 4446的碳质球粒陨石母岩可以考虑与含Au和Pt的Fe、Ni、Co和Cu矿物矿化。这意味着,我们可以预期上述金属和硫化物的天然形式沉积在CV群- c型小行星的碳质球粒陨石母岩上。
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引用次数: 0
Analiza rozwoju leja depresji odkrywki węgla brunatnego Tomisławice w latach 2009–2019 i jego wpływu na stosunki gruntowo-wodne Pojezierza Kujawskiego 2009-2019年Tomisławice褐煤挖掘漏斗的发展及其对Kujawskie湖区水土关系的影响分析
Q4 Earth and Planetary Sciences Pub Date : 2022-08-03 DOI: 10.7306/2022.18
J. Przybyłek
Analysis of the development of the depression cone of the Tomis³awice lignite open pit mine in 2009–2019 and its impact on the soil and water relations of the Kujawy Lakeland. Geol., 70: 527–542; doi: 10.7306/2022.18 A b s t r a c t. The Tomis³awice lignite deposit is located in the Kujawy Lakeland (central Poland), on the water-shed between the Noteæ River (including Gop³o Lake) and the Zg³owi¹czka River (including Lake G³uszyñskie) catchment areas. The dewatering began in January 2009. In June 2011, the lignite seam was uncovered. The deposit was formed in a local Mesozoic depression within a tectonic structure, copmosed of Upper Cretaceous fractured marls. The average thickness of the lignite seam is about 7 m. All the boundaries of the Tomis³awice deposit are ero-sional. The top of the lignite seam, which is lowered to the north is at the average depth of between 38.3 m and 46.8 m. In the study area of the Kujawy Lakeland, groundwater with mineralization of up to 1g/dm 3 occurs down to a depth of 200 m in the Quaternary, Neogene-Paleogene, Cretaceous and Jurassic aquifers in the SE part of the area. The paper provides an analysis of the mine dewatering impact on aquifers within the cone of depression, over 270 km 2 in area, and the mine water drainage rate up to 90 m 3 /min. It is based on the data from the monitoring of the soil and water environment from 2008–2019 (groundwater, lakes). The analysis showed a particular mine dewatering impact of the developmnent of the Upper Cretaceous aquifer on the large-scale cone of depression around the Tomis³awice open pit mine. The described situation caused the mass drying up of farm wells and wetlands over a distance of up to 9 km from the open pit. The groundwater level on the moraine plateau has been almost completely drained and only to a small extent can it be periodically restored after longer periods of heavy rainfall.
2009-2019年Tomis³awice褐煤露天矿凹锥发育及其对库贾维湖区水土关系的影响分析青烟。中文信息学报,70:527-542;Tomis³awice褐煤矿床位于Kujawy Lakeland(波兰中部),位于Noteæ河(包括Gop³o湖)和Zg³owi¹czka河(包括G³uszyñskie湖)集水区之间的分水岭上。脱水开始于2009年1月。2011年6月,褐煤煤层被发现。矿床形成于局部中生代坳陷内的构造构造中,由上白垩统碎裂泥灰岩组成。褐煤煤层平均厚度约为7 m。Tomis³awice矿床的所有边界都是侵蚀性的。褐煤煤层顶部向北降低,平均深度为38.3 ~ 46.8 m。库贾维湖区研究区东南部第四纪、新近系—古近系、白垩系和侏罗系含水层中存在深度200 m以下矿化度高达1g/dm 3的地下水。本文分析了矿井脱水对凹锥内含水层的影响,面积超过270 km2,矿井排水速率高达90 m3 /min。它基于2008-2019年土壤和水环境(地下水、湖泊)的监测数据。分析表明,上白垩统含水层的发育对Tomis³awice露天矿周围的大型凹陷锥有特殊的矿井脱水影响。上述情况造成了距离露天矿9公里范围内的农田水井和湿地大面积干涸。冰碛高原的地下水位几乎已经完全枯竭,在较长时间的强降雨后,只能在很小程度上周期性地恢复。
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引用次数: 0
Wstępna ocena możliwości pozyskiwania pierwiastków wartościowych z wód kopalnianych oraz wód termalnych i leczniczych w Polsce 对从波兰的矿井水、热水和药用水中获取有价值元素的可能性的初步评估
Q4 Earth and Planetary Sciences Pub Date : 2022-07-08 DOI: 10.7306/2022.13
L. Razowska-Jaworek, Marcin Pasternak, M. Karpiński, Z. Będkowski, Z. Kaczorowski, I. Wysocka, P. Drzewicz
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引用次数: 0
Analiza zmian warunków gruntowo-wodnych we Wrocławiu w odniesieniu do klas agresywności wód podziemnych na podstawie danych archiwalnych 根据档案数据分析弗罗茨瓦夫地下水条件变化与地下水侵蚀性等级的关系
Q4 Earth and Planetary Sciences Pub Date : 2022-07-08 DOI: 10.7306/2022.14
Marta Trałka, Marek Błachowicz
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引用次数: 0
Morena szaflarska w świetle nowych danych z odsłonięć i wierceń w 100-lecie jej odkrycia 西伯利亚冰碛发现100周年之际,根据曝光和钻探的新数据
Q4 Earth and Planetary Sciences Pub Date : 2022-07-08 DOI: 10.7306/2022.15
A. Wójcik
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引用次数: 0
Wpływ przerostów piaszczystych w węglu brunatnym na działalność górniczą – przykład ze złoża „Pątnów IV” (okolice Konina) w środkowej Polsce 褐煤中沙子过度生长对采矿活动的影响——以波兰中部Pãtnów IV矿床(科宁地区)为例
Q4 Earth and Planetary Sciences Pub Date : 2022-06-23 DOI: 10.7306/2022.11
Mariusz Dziamara, Veronika Glacová, Jakub Klęsk, Marian Marschalko, R. Wachocki, M. Widera
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引用次数: 2
Wybrane pierwiastki śladowe w górnopermskich (cechsztyn) utworach solnych i potasonośnych w Polsce – ocena złożowa 波兰上巴伐利亚盐矿和钾盐矿床中选定的微量元素——综合评估
Q4 Earth and Planetary Sciences Pub Date : 2022-06-23 DOI: 10.7306/2022.12
G. Czapowski, H. Tomassi-Morawiec, J. Wachowiak
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引用次数: 0
Określanie zmienności mineralogicznej utworów kajpru za pomocą metod petromagnetycznych 用岩石磁学方法测定kajper块的矿物学变异性
Q4 Earth and Planetary Sciences Pub Date : 2022-04-21 DOI: 10.7306/2022.10
Kamil Kobyliński
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Przeglad Geologiczny
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