山西介休洪山钙华的空间分布特征、成因及时代探讨

P931.5%P642.25; 地处山西省介休市洪山镇狐岐山脚下的钙华,是山西省内娘子关钙华景观之外的又一具有观赏潜质的岩溶景观.其出露范围较大,厚度稳定,形态优美,具有较高的旅游地质观赏价值.文章对洪山钙华进行了系统的地质调查和剖面实测,对钙华的分布范围、产出状态、岩石特征、岩石化学特征、地球化学特征及同位素年代等进行了研究,并从洪山泉岩溶水系统循环的角度,探讨了钙华的形成机理、影响因素及形成时代,可为该区钙化的保护和景观开发提供科学依据....

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Published in中国岩溶 Vol. 40; no. 3; pp. 389 - 397
Main Authors 魏荣珠, 韩颖, 胥勤勉, 魏云峰, 杜艳伟, 范俊辉
Format Journal Article
LanguageChinese
Published 山西省地质调查院,山西 太原 030006%中国地质调查局天津地质调查中心,天津 300170 01.06.2021
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ISSN1001-4810
DOI10.11932/karst2021y004

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Abstract P931.5%P642.25; 地处山西省介休市洪山镇狐岐山脚下的钙华,是山西省内娘子关钙华景观之外的又一具有观赏潜质的岩溶景观.其出露范围较大,厚度稳定,形态优美,具有较高的旅游地质观赏价值.文章对洪山钙华进行了系统的地质调查和剖面实测,对钙华的分布范围、产出状态、岩石特征、岩石化学特征、地球化学特征及同位素年代等进行了研究,并从洪山泉岩溶水系统循环的角度,探讨了钙华的形成机理、影响因素及形成时代,可为该区钙化的保护和景观开发提供科学依据.
AbstractList P931.5%P642.25; 地处山西省介休市洪山镇狐岐山脚下的钙华,是山西省内娘子关钙华景观之外的又一具有观赏潜质的岩溶景观.其出露范围较大,厚度稳定,形态优美,具有较高的旅游地质观赏价值.文章对洪山钙华进行了系统的地质调查和剖面实测,对钙华的分布范围、产出状态、岩石特征、岩石化学特征、地球化学特征及同位素年代等进行了研究,并从洪山泉岩溶水系统循环的角度,探讨了钙华的形成机理、影响因素及形成时代,可为该区钙化的保护和景观开发提供科学依据.
Author 魏荣珠
胥勤勉
范俊辉
杜艳伟
魏云峰
韩颖
AuthorAffiliation 山西省地质调查院,山西 太原 030006%中国地质调查局天津地质调查中心,天津 300170
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WEI Yunfeng
WEI Rongzhu
HAN Ying
FAN Junhui
DU Yanwei
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Title 山西介休洪山钙华的空间分布特征、成因及时代探讨
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