Diagenesis of spiculites and carbonates in a Permian temperate ramp succession – Tempelfjorden Group, Spitsbergen, Arctic Norway

Matysik Micha?; Stemmerik Lars; Olaussen Snorre; Brunstad Harald; Betzler Christian

摘要

Abstract > This paper explores little investigated diagenesis of spicule‐dominated sediments, based on Permian spiculites and cool‐water carbonates of the Tempelfjorden Group in central Spitsbergen. Field observations, petrography, stable isotope geochemistry, and mineralogical and chemical analyses reveal that the strata have been subjected to multistage diagenesis as the result of silica phase transitions at medium burial depths and deep‐burial overprinting. The growth of silica concretions occurred during the opal‐A/opal‐ <fc>CT</fc> conversion and was controlled by the content and distribution of clay and spicules in the sediment, resulting in a variety of megascopic silica fabrics. Opal‐ <fc>CT</fc> was subsequently dissolved, and all silica is now in a stable quartz stage. Petrographically, the rocks are characterized by a variety of chalcedony and quartz cements which perfectly preserve precursor textures. Most cements precipitated from silica‐oversaturated fluids, and their shapes reflect the silica saturation state and geometry of the pore space. Some microquartz and cryptoquartz also formed by a solid–solid inversion (recrystallization) of chalcedony. The cements have δ 18 O values between +30‰ and +20‰ Standard Mean Ocean Water and display a systematic depletion in 18 O from the first to the last crystallized, interpreted to reflect a gradual increase in temperature during burial. The precipitation of quartz cements started in the Middle Triassic when the strata passed the 19°C isotherm at burial depths of ca 600?m, and was completed in the mid‐Cretaceous, 2·3?km beneath the sea floor at temperatures of 75°C. Late diagenetic overprinting of the cher </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“sed12404-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</标题> >本文探讨了基于中央孢子菌灌木丛组的二叠纪刺激物和冷水碳酸盐的沉积物的少量研究成岩作用。现场观测，岩画，稳定同位素地球化学和矿物学和化学分析表明，由于中埋深度和深埋叠印的二氧化硅相转变的结果，地层已经进行了多级成岩作用。在蛋白石-A / OPAL-<FC>转化期间发生二氧化硅凝集的生长，并通过沉积物中粘土的含量和分布和分布来控制，导致各种兆型二氧化硅织物。随后溶解蛋白质-<Fc> CT </ Fc>，所有二氧化硅现在处于稳定的石英阶段。岩石地上，岩石的特征在于各种氨化细菌和石英水泥，完全保持前体纹理。大多数水泥从二氧化硅过饱和流体中沉淀出来，它们的形状反射了孔隙空间的二氧化硅饱和状态和几何形状。一些微型和加密型也由氨化的固体固体反转（再结晶）形成。水泥具有+ 30°和+ 20℃之间的+ 30×和+ 20℃之间的+ 30°和+ 20℃之间的δ118。首先是最后结晶，解释为在埋葬期间反映温度逐渐增加。当阶层在埋藏深度在 Ca </ i> 600？m的埋藏深度通过19°C等温线时，在中间三叠系中开始了石英水泥的沉淀，并在中白垩统完成，2·3？Km下方海底在75°C的温度下。雪儿的后期成岩套印 </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-28547/'>《Sedimentology: Journal of the International Association of Sedimentologists》</a> <b style="margin: 0 2px;">|</b><span>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共30页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Matysik Micha?&option=202" target="_blank" rel="nofollow">Matysik Micha?;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stemmerik Lars&option=202" target="_blank" rel="nofollow">Stemmerik Lars;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Olaussen Snorre&option=202" target="_blank" rel="nofollow">Olaussen Snorre;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brunstad Harald&option=202" target="_blank" rel="nofollow">Brunstad Harald;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Betzler Christian&option=202" target="_blank" rel="nofollow">Betzler Christian;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Natural History MuseumUniversity of Copenhagen?ster Voldgade 5–7 DK‐1350 Copenhagen K Denmark;</p> <p>Natural History MuseumUniversity of Copenhagen?ster Voldgade 5–7 DK‐1350 Copenhagen K Denmark;</p> <p>The University Centre in Svalbard (UNIS)P.O. Box?156 N‐9171 Longyearbyen Norway;</p> <p>Lundin Norway ASStrandveien 4 P.O. Box?247 N‐1326 Lysaker Norway;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/165.html" title="地质学">地质学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Burial diagenesis&option=203" rel="nofollow">Burial diagenesis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=chert&option=203" rel="nofollow">chert;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Permian&option=203" rel="nofollow">Permian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=quartz cement&option=203" rel="nofollow">quartz cement;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=silicification&option=203" rel="nofollow">silicification;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=spicule diagenesis&option=203" rel="nofollow">spicule diagenesis;</a> </p> <div class="translation"> 机译：埋葬成岩作用;燧石;二叠纪;石英水泥;硅化;乳酪成岩作用; 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