最近30从www.hoelymoley.com 2023 - 07 - 07 - t21:36:48z //www.hoelymoley.com/feeds/question/15921 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/15921 5 马丁 //www.hoelymoley.com/users/14748 2019 - 01 - 09 - t22:53:40z 2019 - 08 - 28 - t07:44:41z

< p >我把这些照片匆忙(抱歉,颜色有点由于低光,第一张照片是最扭曲的一个)。< / p > < p >,这让我皮肤颜色似乎遵循岩石的裂缝。有人能解释我沿着凹槽的红棕色颜色引起的吗?< / p > < p > IIRC非常抛光流纹岩,显示的基石,位置是< a href = " https://www.google.it/maps/place/Gleifkirche/@46.4551142, 11.249813, 725 " rel = " noreferrer " >“意大利Eppan Gleif教堂”< / >。进一步的研究告诉我,发生了冰川抛光< a href = " https://en.wikipedia.org/wiki/W%C3%BCrm_glaciation " rel = " noreferrer " > < / >的玉木冰川时期,结束于12000年前。< / p > < p > < a href = " https://i.stack.imgur.com/fAixa.jpg " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/fAixa.jpg " alt = "在这里输入图像描述" > < / > < / p > < p > < a href = " https://i.stack.imgur.com/yofAE.jpg " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/yofAE.jpg " alt = "在这里输入图像描述" > < / > < / p > < p > < a href = " https://i.stack.imgur.com/MNyki.jpg " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/MNyki.jpg " alt = "在这里输入图像描述" > < / > < / p > < p > < a href = " https://i.stack.imgur.com/4YZR1.jpg " rel = " noreferrer " > < img src = " https://i.stack.imgur.com/4YZR1.jpg " alt = "在这里输入图像描述" > < / > < / p >

//www.hoelymoley.com/questions/15921/-/15958 # 15958 3 MyCarta //www.hoelymoley.com/users/144 2019 - 01 - 14 t22:41:36z 2019 - 01 - 14 t22:41:36z

< p >这个答案是基于粗略地看看1:5万< a href = " http://www.isprambiente.gov.it/Media/carg/26_APPIANO/Foglio.html " rel = " nofollow noreferrer " >瑞奇亮相< / >,地质图的意大利(意大利语言,据我所知)。我在评论中指出,我意愿它作为进一步的调查只是一个开始,应该做更详细的地质工作和可能更多的领域工作。我建议联系办公室< a href = " http://www.provincia.bz.it/costruire-abitare/edilizia-pubblica/rilevamento-geologico-e-geotematico.asp " rel = " nofollow noreferrer " >的地质调查局Provincia迪博尔扎诺< / >他们肯定知道该地区好,可以打电话或者通过电子邮件回答。< / p > < p >这是我认为,基于我粗略的看。< / p > < p >截面C走~南临Cornaiano镇以北,相对靠近教堂的位置,也就是西方的圣米歇尔(基于谷歌地图链接);我表示它的近似下落在下图黄色的圆圈。它看起来像你的照片可能是一个露头的岩石的奥拉(在图中橙色),形成一个流纹岩火山凝灰岩的< em > Atesino组< / em >。< / p > < p > < a href = " https://i.stack.imgur.com/sOnjX.png " rel = " nofollow noreferrer " > < img src = " https://i.stack.imgur.com/sOnjX.png " alt = "在这里输入图像描述" > < / > < / p > < p >的< em >模式tettonico < / em >下面(寻找亮相)显示了< em > Atesino火山群< / em >和接触是一个很有沉积剖面(< em > Successione sedimentaria permocenozoica < / em >);我想说地热流体循环通过这些骨折导致热液蚀变的表面是一个合理的解释你捕捉到的颜色。< a href = " https://i.stack.imgur.com/jB5Z0.jpg " rel = " nofollow noreferrer " > < img src = " https://i.stack.imgur.com/jB5Z0.jpg " alt = "在这里输入图像描述" > < / > < / p >

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