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33.
Petrogenesis of the Ulsan carbonate rocks from the south-eastern Kyongsang Basin, South Korea 总被引:1,自引:0,他引:1
Abstract The petrogenesis of the Ulsan carbonate rocks in the Mesozoic Kyongsang Basin of South Korea, which have previously been interpreted as limestone of Paleozoic age, is reconsidered in the present study. Within the Kyongsang Basin, a small volume of carbonate rocks, containing a magnetite deposit and spatially associated ultramafic rocks, is surrounded by sedimentary, volcanic and granitic rocks of the Mesozoic age. The simple cross‐cutting relationships and other outcrop features of the area indicate that the carbonate rocks are an intrusive phase and younger than the other surrounding Mesozoic rocks. The Ulsan carbonates have low concentrations of rare earth elements (REE) and trace elements with the carbon and oxygen isotope values in the range of δ13CPDB = 2.4 to 4.0‰ and δ18OSMOW = 17.0 to 19.5‰. Outcrop evidence and geochemical signatures indicate that the Ulsan carbonates were formed from crustal carbonate melts, which were generated by the melting/fluxing of crustal carbonate materials, caused by the emplacement‐related processes of alkaline A‐type granitic rocks. Compared to typical mantle‐derived carbonatites associated with silica‐undersaturated, strongly peralkaline systems, the relatively small size and geochemical characteristics of the Ulsan carbonates reflect carbonatite genesis in a silica‐saturated, weakly alkali intrusive system. Major deep‐seated tectonic fractures formed by the collapse of the cauldron or the rift system associated with the opening of the East Sea (Japan Sea) might have facilitated the ascent of the crustal carbonate melts. 相似文献
34.
碳酸盐与陆源碎屑的混合沉积研究至今尚未引起足够重视。文献屈指可数。扬子西经缘龙门山地区盆纪发育了了这类良好的混合沉积。作者根据实际材料,首次从这一思路出发,识别该区泥盆纪Emsian期到Givetian早期的混积相四种,混积亚相约14种,阐明了其优势混积作用;根据混积作用特征、沉积背景关系,划分出两大混积类型,即泥质背景下的混积1型和砂灰质背景下的混积Ⅱ型;对混积作用机理进行了探讨;并指出不同级次 相似文献
35.
黔南Triticites带旋回层序碳同位素特征及冰川型海平面变化 总被引:4,自引:0,他引:4
应用层序地层学理论对黔南独山地区晚石炭世麦粒链带地层进行了详细的沉积层序分析和系统的碳同位素测定,识别出2个三级沉积层序和17个准层序,其可与北美中大陆同期地层中发现的2个三级沉积层序和17个亚层序对比,是晚石炭世Gzhelian期存在全球沉积记录同时性的佐证。同时探讨了碳同位素演化与全球海平面变化之间的内在联系,总结出沉积层序内碳同位素演化规律。 相似文献
36.
This paper deals with dissolved inorganic carbon (DIC) and organic carbon (DOC) in pore waters from a 150 m deep hole drilled through the carbonate barrier reef of Tahiti and its underlying basalt basement. Alkalinity-pH measurements were used to calculate the DIC species concentration, and DOC was analysed according to the high temperature catalytic oxidation technique. Salinity was used as a conservative tracer to help identify water origin and mixing within the hole. Water mixing, calcium carbonate dissolution and mineralization of organic carbon combined to form three distinct groups of pore water. In the deeper basalt layers, pore water with alkalinity of 1.4 meq kg–1 pH of 7.6 and p(CO2) of 1.2 mAtm was undersaturated with respect to both aragonite and calcite. In the intermediate carbonate layer, pore water with alkalinity of more than 2.0 meq kg–1, pH of 7.70 and p(CO2) of 1.4 mAtm was supersaturated with respect to both aragonite and calcite. The transition zone between those two groups extended between 80 and 100 m depth. The shift from aragonite undersaturation to supersaturation was mainly attributed to the mixing of undersaturated pore waters from the basalt basement with supersaturated pore waters from the overlaying limestone. In the top of the reef, inputs from a brackish water lens further increased p(CO2) up to 5.6 times the atmospheric P(CO2). 相似文献
37.
Wolfgang H. Berger Memorie K. Yasuda Torsten Bickert Gerold Wefer 《International Journal of Earth Sciences》1996,85(3):466-495
We provide a reconstruction of atmospheric CO2 from deep-sea sediments, for the past 625000 years (Milankovitch chron). Our database consists of a Milankovitch template
of sea-level variation in combination with a unique data set for the deep-sea record for Ontong Java plateau in the western
equatorial Pacific. We redate the Vostok ice-core data of Barnola et al. (1987). To make the reconstructions we employ multiple
regression between deep-sea data, on one hand, and ice-core CO2 data in Antarctica, on the other. The patterns of correlation suggest that the main factors controlling atmospheric CO2 can be described as a combination of sea-level state and sea-level change. For best results squared values of state and change
are used. The square-of-sea-level rule agrees with the concept that shelf processes are important modulators of atmospheric
CO2 (e.g., budgets of shelf organic carbon and shelf carbonate, nitrate reduction). The square-of-change rule implies that, on
short timescales, any major disturbance of the system results in a temporary rise in atmospheric CO2. 相似文献
38.
Chr Samtleben A. Munnecke T. Bickert J. Pätzold 《International Journal of Earth Sciences》1996,85(2):278-292
The Silurian of Gotland, Sweden, consists of 440 m of carbonate deposits. Repeatedly, uniform sequences of micritic limestones
and marls are interrupted by complex-structured reefs and by adjacent platform sediments. Generally, the alteration of facies
is interpreted as the result of sea-level fluctuations caused by a gradual regression with superimposed minor transgressive
pulses. The purpose of this study is a facies interpretation based on both field observations and stable isotope measurements
of brachiopod shells. Approximately 700 samples from stratigraphically arranged localities in different facies areas have
been investigated. The carbon and oxygen isotopes show principally parallel curves and a close relationship to the stratigraphic
sequence. Lower values occur in periods dominated by deposition of marly sequences. Higher values are observed in periods
dominated by reefs and extended carbonate platforms. The oxygen isotope ratios are interpreted to reflect paleosalinity changes
due to varying freshwater input, rather than to paleotemperature. Carbon isotope ratios are believed to have been connected
to global changes in the burial of organic carbon in black shales during periods of euxinic deep water conditions. Consequently,
the facies succession on Gotland results from global paleoclimatic conditions. Changes in terrigenous input due to different
rates of weathering and freshwater runoff, rather than sea-level fluctuations, control the carbonate formation of the Silurian
on Gotland. 相似文献
39.
形成岩溶的高阻碳酸盐岩对电磁波的吸收较弱,而且成层沉积的特定环境使碳酸盐岩地区岩石的各向异性现象较明显,由于地空界面的存在及岩溶洞壁两侧介质电性差异明显,界面清晰,又使电磁波出现强烈的反射及散射现象,从理论上对碳酸盐岩地区电磁波传播的特有现象进行了研究和分析,并给出结论。 相似文献
40.
碳酸盐岩的反射光谱特征的研究及应用 总被引:2,自引:0,他引:2
在室内对新疆塔里木盆地西北缘柯坪地区碳酸盐岩的反射光谱进行了测量。分析结果表明:碳酸盐岩的特征吸收谱带位于2300~2350nm,随着碳酸盐岩中Mg2+含量的增加,其特征吸收谱带的中心波长位置具有向短波长方向移动的特点;同时,随着碳酸盐岩中碳酸盐矿物含量的增加,其特征吸收谱带的深度(D)也有增大的趋势,并且岩石的平均反射率(R)也随着增高。根据这些特征可以判定碳酸盐岩的岩石类型及碳酸盐矿物的相对含量 相似文献