{"id":8552,"date":"2018-02-07T14:42:55","date_gmt":"2018-02-07T13:42:55","guid":{"rendered":"http:\/\/igcas.antstudio.eu\/contact\/staff\/lenka-spicakova\/"},"modified":"2024-02-12T14:35:27","modified_gmt":"2024-02-12T13:35:27","slug":"lenka-spicakova","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/lenka-spicakova\/","title":{"rendered":"Lenka \u0160pi\u010d\u00e1kov\u00e1"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;20px|0px|0px|0px&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row column_structure=&#8221;2_3,1_3&#8243; _builder_version=&#8221;4.16&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; custom_padding=&#8221;19px|0px|24px|0px&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.23.1&#8243; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><strong>Lenka \u0160pi\u010d\u00e1kov\u00e1<\/strong> is research and development expert at the Institute of Geophysics of the Czech Academy of Sciences.<\/p>\n<p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.23.1&#8243; hover_enabled=&#8221;0&#8243; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h3><strong>Publications<\/strong><\/h3>\n<ul>\n<li><strong>\u0160pi\u010d\u00e1kov\u00e1, L.<\/strong> &amp; Uli\u010dn\u00fd, D., 2014. Phases of the mid-Cenomanian transgression recorded in a\u00a0composite palaeovalley fill \u2013 the Horou\u0161any quarry, Bohemian Cretaceous Basin. In: Cretaceous Basins of Central Europe, edited by: M. Wilmsen, D. Uli\u010dn\u00fd and M. Ko\u0161\u0165\u00e1k. Zeitschrift des deutchen Gesselschafts der Geowissenschaften, 12, 165(4), pp. 591-619. DOI: <a href=\"http:\/\/dx.doi.org\/10.1127\/zdgg\/2014\/0028\">10.1127\/zdgg\/2014\/0028<\/a><\/li>\n<li>Uli\u010dn\u00fd, D., L.\u00a0<strong>\u0160pic\u00e1kov\u00e1<\/strong>, R. Grygar, M. Svobodov\u00e1, S. \u010cech and J. Laurin (2009), Palaeodrainage systems at the basal unconformity of the Bohemian Cretaceous Basin: Roles of inherited fault systems and basement lithology during the onset of basin filling, Bulletin of Geosciences 84 (4) , pp. 577-610, <a href=\"http:\/\/www.geology.cz\/bulletin\/fulltext\/1128_ulicny.pdf\" target=\"_blank\" rel=\"noopener\">link<\/a>.<\/li>\n<li><strong>\u0160pi\u010d\u00e1kov\u00e1<\/strong>, L., D. Uli\u010dn\u00fd, and G. Koudelkov\u00e1 (2000). Tectonosedimentary evolution of the Cheb Basin (NW Bohemia, Czech Republic) between Late Oligocene and Pliocene: a&nbsp;preliminary note. Studia Geophysica et Geodaetica, v. 44, p.&nbsp;556-580, DOI:\u00a0<a href=\"http:\/\/www.ig.cas.cz\/tektonika-geodynamika\/%20http:\/\/link.springer.com\/article\/10.1023%2FA%3A1021819802569\" target=\"_blank\" rel=\"noopener\">10.1023\/A:1021819802569<\/a>.<\/li>\n<li>Uli\u010dn\u00fd, D., J. Kva\u010dek, M. Svobodov\u00e1, and L.\u00a0<strong>\u0160pi\u010d\u00e1kov\u00e1<\/strong>\u00a0(1997). High-frequency sea-level fluctuations and plant habitats in cenomanian fluvial to estuarine succession: Pecinov quarry, Bohemia, Palaeogeography, Palaeoclimatology, Palaeoecology 136 (1-4) , pp. 165-197, DOI:\u00a0<a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S0031018297000333\" target=\"_blank\" rel=\"noopener\">10.1016\/S0031-0182(97)00033-3<\/a>.<\/li>\n<li>Uli\u010dn\u00fd, D. and L.\u00a0<strong>\u0160pi\u010d\u00e1kov\u00e1<\/strong>\u00a0(1996). Response to high-frequency sea-level change in a&nbsp;fluvial to estuarine succession: Cenomanian paleovalley fill, Bohemian Cretaceous Basin. In: J. A. Howell and J. F. Aitken.(eds.): High-resolution Sequence Stratigraphy: Innovations and Applications. Geological Society Special Publication 104, p.&nbsp;247-268. The Geological Society, London.<\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/ls-portret2.jpg&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;center&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.16&#8243; max_width=&#8221;60%&#8221; module_alignment=&#8221;center&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.23.1&#8243; text_font=&#8221;||||||||&#8221; text_line_height=&#8221;0.5em&#8221; header_font=&#8221;||||||||&#8221; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h3 style=\"text-align: center;\"><strong>RNDr. Lenka \u0160pi\u010d\u00e1kov\u00e1 Ph.D.<\/strong><\/h3>\n<p style=\"text-align: center;\">research and development expert<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/surface-processes-palaeoclimate\/\">Surface Processes &amp; Palaeoclimate<\/a><\/p>\n<p style=\"text-align: center;\"><a href=\"mailto:spicka@ig.cas.cz\">spicka@ig.cas.cz<\/a><\/p>\n<p style=\"text-align: center;\">+420&nbsp;267&nbsp;103&nbsp;343<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.researcherid.com\/rid\/H-6406-2014\">ResearcherID<\/a><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Lenka \u0160pi\u010d\u00e1kov\u00e1 is research and development expert at the Institute of Geophysics of the Czech Academy of Sciences.Publications \u0160pi\u010d\u00e1kov\u00e1, L. &amp; Uli\u010dn\u00fd, D., 2014. Phases of the mid-Cenomanian transgression recorded in a\u00a0composite palaeovalley fill \u2013 the Horou\u0161any quarry, Bohemian Cretaceous Basin. In: Cretaceous Basins of Central Europe, edited by: M. Wilmsen, D. Uli\u010dn\u00fd and M. [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":12002,"parent":416,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[127],"class_list":["post-8552","page","type-page","status-publish","has-post-thumbnail","hentry","tag-people-en"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Lenka \u0160pi\u010d\u00e1kov\u00e1 - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/lenka-spicakova\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Lenka \u0160pi\u010d\u00e1kov\u00e1 - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"Lenka \u0160pi\u010d\u00e1kov\u00e1 is research and development expert at the Institute of Geophysics of the Czech Academy of Sciences.Publications \u0160pi\u010d\u00e1kov\u00e1, L. &amp; Uli\u010dn\u00fd, D., 2014. Phases of the mid-Cenomanian transgression recorded in a\u00a0composite palaeovalley fill \u2013 the Horou\u0161any quarry, Bohemian Cretaceous Basin. In: Cretaceous Basins of Central Europe, edited by: M. Wilmsen, D. Uli\u010dn\u00fd and M. 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