米粒状白云石及其出溶成因

邬金华; Philip Fralick

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米粒状白云石及其出溶成因

邬金华, Philip Fralick

文章导航 > 沉积学报 > 1992 > 10(2): 45-53

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

引用本文:

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

Citation:

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

引用本文:

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

Citation:

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

米粒状白云石及其出溶成因

1.
中国地质大学地质系, 武汉;
2.
Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

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文章访问数: 570
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Rice-shaped Dolomite and Its Exsolution Origin

1.
China University of Geosciences;
2.
Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

摘要

摘要: 米粒状白云石产于奥陶系近岸碳酸盐岩序列的云斑(生屑)泥晶灰岩、砾屑灰岩和叠层石灰岩中,在虫孔和砾屑粒间最为富集,外形为伸长菱面体,薄片中呈米粒状.晶体无环带或雾心,但内部含大量呈规则分布的细小方解石“包体”,结晶C轴垂直于晶体延长方向.与背景方解石泥晶相比,Fe、Mn、Na和Ba含量较高,Sr含量较低.C轴的固定取向排除了石膏假晶的可能,也不是普通白云石化或交代钡白云石的结果,推测是沉淀镁方解石重结晶后在压力增加的条件下经出溶作用形成.
- 镁方解石 /
- 重结晶 /
- 出溶作用 /
- 米粒状白云石
Abstract: Rice- shaped dolomite crystals exist in dolomite- patched micritic, biomicritic, intraclastic andstrornatolitic limestones in an Ordovician nearshore, carbonate succession, reaching their highest concen-trations promixal to worm burrows and pore space between intraclasts. The crystals are elongaterhombohedra and appear to be elongate hexagons, parallelograms or trapezoids and look like rice grains inthin sections. No internal zoning or foggy cores are present but numc;rous minute calcite "enclusions" distrib-ute parallel to the boundary of the crystals. The C-axis is perpendicular to the longer boundary of the crystalIt contains higher Fe, Mn, Na and Ba than surrounding calcite micrite which contains a greater proportion of Sr, especially its Fe and Ba are tens of times higher than those of calcite. C-axis orientation negatesthe dolomite representing replacement of gypsum.It can not be ureated by an ordinary dolomitization or thereplacement of norsethite and is suggested to form in a process that the precipitated magnesian calcite.is recrystallized into its inherent crystallographic shape, then followed by exsolution accompanied by ex-change of calcium for magnesium ions under conditions of increased pressure. The agent triggering therecrystallization of magnesian calcite is probablyinpenecontamporaueous of early diagenetie interstitial wat er with high Mg/‘Ca ratio, in which there may be some substance that can release chemical energy not on、to dehydrate Mg²⁺ but also to order the entering of the ions into lattice. As the water solution permeates thesediments downward and upper layers are dolomitized, the substance (or its energel is consumed gridnally, the concentration of which could become as less as can only carry out dehydration of Ioci1 ion, but cat not make the activity of the cans ordered whrn the solution reaches the lower livers, As a result, parts，mignesian calcite in the lower sediments ire favoured to grow up trir;sforming W their inheren}rvstallographic shape. Some $a compound seems to be a candidate 1-or the substance

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参考文献(1)

[1]

(1) 莫柔，D.W., 1983，国外地质科技(地矿物情报研究所)，1984年第6期，3-13页，第7期，1-13页

(2) 邬金华，1989，出溶白云石，地质科技情报(中国地质大学)，第色期，3I-34页.

(3) Althoff, P.L., 1977, Amer. Mineral., V.62, p.772-783.

(4) Blatt, H.，Middleton, G. and Murray, R.，1980, Origin of sedimentary rocks,Hall, Englewood Cliffs New Jersey p.782.

(5) Goldsmith J., 1960, Jour. of Geology. V.68, p.103-109:

(6) Land, L.S. and Epstein, S., 1970, Sedimentology, V.14, p.187-2D0.

(7) Lippmann, F.> 1973, Sedimentary carbonate minerals, Springer-Verl,ag. New York.second edition. Prenticep.228.

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文章访问数: 570
HTML全文浏览量: 12
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米粒状白云石及其出溶成因

1. 中国地质大学地质系, 武汉;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

收稿日期: 1990-06-30
刊出日期: 1992-06-10

关键词:

镁方解石 /

重结晶 /

出溶作用 /

米粒状白云石

摘要: 米粒状白云石产于奥陶系近岸碳酸盐岩序列的云斑(生屑)泥晶灰岩、砾屑灰岩和叠层石灰岩中,在虫孔和砾屑粒间最为富集,外形为伸长菱面体,薄片中呈米粒状.晶体无环带或雾心,但内部含大量呈规则分布的细小方解石“包体”,结晶C轴垂直于晶体延长方向.与背景方解石泥晶相比,Fe、Mn、Na和Ba含量较高,Sr含量较低.C轴的固定取向排除了石膏假晶的可能,也不是普通白云石化或交代钡白云石的结果,推测是沉淀镁方解石重结晶后在压力增加的条件下经出溶作用形成.

English Abstract

Rice-shaped Dolomite and Its Exsolution Origin

1. China University of Geosciences;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

Received Date: 1990-06-30
Publish Date: 1992-06-10

Abstract: Rice- shaped dolomite crystals exist in dolomite- patched micritic, biomicritic, intraclastic andstrornatolitic limestones in an Ordovician nearshore, carbonate succession, reaching their highest concen-trations promixal to worm burrows and pore space between intraclasts. The crystals are elongaterhombohedra and appear to be elongate hexagons, parallelograms or trapezoids and look like rice grains inthin sections. No internal zoning or foggy cores are present but numc;rous minute calcite "enclusions" distrib-ute parallel to the boundary of the crystals. The C-axis is perpendicular to the longer boundary of the crystalIt contains higher Fe, Mn, Na and Ba than surrounding calcite micrite which contains a greater proportion of Sr, especially its Fe and Ba are tens of times higher than those of calcite. C-axis orientation negatesthe dolomite representing replacement of gypsum.It can not be ureated by an ordinary dolomitization or thereplacement of norsethite and is suggested to form in a process that the precipitated magnesian calcite.is recrystallized into its inherent crystallographic shape, then followed by exsolution accompanied by ex-change of calcium for magnesium ions under conditions of increased pressure. The agent triggering therecrystallization of magnesian calcite is probablyinpenecontamporaueous of early diagenetie interstitial wat er with high Mg/‘Ca ratio, in which there may be some substance that can release chemical energy not on、to dehydrate Mg²⁺ but also to order the entering of the ions into lattice. As the water solution permeates thesediments downward and upper layers are dolomitized, the substance (or its energel is consumed gridnally, the concentration of which could become as less as can only carry out dehydration of Ioci1 ion, but cat not make the activity of the cans ordered whrn the solution reaches the lower livers, As a result, parts，mignesian calcite in the lower sediments ire favoured to grow up trir;sforming W their inheren}rvstallographic shape. Some $a compound seems to be a candidate 1-or the substance

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

引用本文:

邬金华, Philip Fralick. 米粒状白云石及其出溶成因[J]. 沉积学报, 1992, 10(2): 45-53.

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

Citation:

Wu Jinhua, Philip Fralick. Rice-shaped Dolomite and Its Exsolution Origin[J]. Acta Sedimentologica Sinica, 1992, 10(2): 45-53.

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米粒状白云石及其出溶成因

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Rice-shaped Dolomite and Its Exsolution Origin

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米粒状白云石及其出溶成因

1. 中国地质大学地质系, 武汉;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

English Abstract

Rice-shaped Dolomite and Its Exsolution Origin

1. China University of Geosciences;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

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米粒状白云石及其出溶成因

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Rice-shaped Dolomite and Its Exsolution Origin

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米粒状白云石及其出溶成因

1. 中国地质大学地质系, 武汉; 2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

English Abstract

Rice-shaped Dolomite and Its Exsolution Origin

1. China University of Geosciences; 2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

全文HTML

目录

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期刊在线

联系我们

1. 中国地质大学地质系, 武汉;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1

1. China University of Geosciences;

2. Geology Department, Lakehead University, Thunder Bay, Ontario, Canada P7B 5E1