{"id":89,"date":"2018-02-16T10:18:00","date_gmt":"2018-02-16T08:18:00","guid":{"rendered":"http:\/\/minsysfin.gtk.fi\/?page_id=89"},"modified":"2020-06-15T14:49:02","modified_gmt":"2020-06-15T11:49:02","slug":"central_lapland_greenstone_belt-2","status":"publish","type":"page","link":"https:\/\/minsysfin.gtk.fi\/index.php\/central_lapland_greenstone_belt-2\/","title":{"rendered":"Central Lapland Greenstone Belt, fault architecture and structural development"},"content":{"rendered":"<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-bottom: 0px;margin-top: 0px;border-width: 0px 0px 0px 0px;border-color:#eae9e9;border-style:solid;\" ><div class=\"fusion-builder-row fusion-row\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_3 1_3 fusion-one-third fusion-column-first\" style=\"width:33.333333333333%;width:calc(33.333333333333% - ( ( 4% ) * 0.33333333333333 ) );margin-right: 4%;margin-top:0px;margin-bottom:20px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 0px 0px;\"><div class=\"fusion-text fusion-text-1\"><p>Most of the known orogenic gold deposits and occurrences in the Central Lapland Greenstone Belt (CLGB) are located along\u00a0 the Kiistala Shear Zone (KiSZ) and the Sirkka Shear Zone (SSZ), as well as along some other shear zones and thrust faults. These zones and faults were re-activated several times during the ~ 150 Ma long Svecofennian (1.92-1.77 Ga) tectonic evolution which included five major stages:<\/p>\n<p>D1 (1.92-1.90 Ga) &#8211; E-W contraction with formation of thrust faults. The Suurikuusikko gold deposit along the Kiistala Line has formed during this stage.<\/p>\n<p>D2 (1.90-1.89 Ga) &#8211; N-S shortening event, where most of the strain was taken up by the northern and southern (SSZ) thrusts.<\/p>\n<p>D3 (1.88-1.87 Ga) &#8211; tectonic vectors were\u00a0switched from N-S to NE-SW and dextral strike-slip regime commenced along the KiSZ.<\/p>\n<p>D4 (1.84-1.81 Ga) &#8211; a near-orthogonal switch of the regional stress regime from NE-SW to NW-SE flipped the kinematics of the KiSZ from dextral to sinistral.<\/p>\n<p>D5 (1.77-1.76 Ga) \u2013 the last deformation phase produced widespread veining under E-W contraction. Accumulation of gold occurred in several deposits at this stage.<\/p>\n<p>Due to the petrophysical differences among formations that have been juxtaposed next to each other along the major shear zones, the pseodogravity worms can be used to map out the potential conduits of fluid flow in the CLGB, which is largely covered by glaciogenic sediments.<\/p>\n<\/div><div class=\"fusion-clearfix\"><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_3_5 3_5 fusion-three-fifth fusion-column-last\" style=\"width:60%;width:calc(60% - ( ( 4% ) * 0.6 ) );margin-top:0px;margin-bottom:20px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 5px 0px 0px 100px;\"><span class=\" fusion-imageframe imageframe-none imageframe-1 hover-type-none\"><a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-1030x561.png\" class=\"fusion-lightbox\" data-rel=\"iLightbox[66a2c44909148059b83]\" data-caption=\"Major faults and orogenic gold deposits in the Central Lapland Greenstone Belt\" data-title=\"Major faults and orogenic gold deposits in the Central Lapland Greenstone Belt\" title=\"Major faults and orogenic gold deposits in the Central Lapland Greenstone Belt\"><img decoding=\"async\" width=\"1030\" height=\"561\" alt=\"Major faults and orogenic gold deposits in the Central Lapland Greenstone Belt\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-1030x561.png\" class=\"img-responsive wp-image-981\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-200x109.png 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-400x218.png 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-600x327.png 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-800x435.png 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Basement_Structures_Deposits_CLGB-1200x653.png 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/a><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:15px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><span class=\" fusion-imageframe imageframe-none imageframe-2 hover-type-none\"><a class=\"fusion-no-lightbox\" href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-scaled.jpg\" target=\"_self\" aria-label=\"Gravity worms\"><img decoding=\"async\" width=\"1030\" height=\"665\" alt=\"Gravity worms\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-1030x665.jpg\" class=\"img-responsive wp-image-1112\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-200x129.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-400x258.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-600x387.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-800x516.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Gravity_worms-1200x775.jpg 1200w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><\/a><\/span><div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-bottom: 0px;margin-top: 0px;border-width: 0px 0px 0px 0px;border-color:#eae9e9;border-style:solid;\" ><div class=\"fusion-builder-row fusion-row\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_1 1_1 fusion-one-full fusion-column-first fusion-column-last\" style=\"margin-top:0px;margin-bottom:20px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 9px 75px 0px 0px;\"><span class=\" fusion-imageframe imageframe-none imageframe-3 hover-type-none\"><a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution.png\" class=\"fusion-lightbox\" data-rel=\"iLightbox[e63bb3bb67980d12c7a]\" data-title=\"Tect evolution\" title=\"Tect evolution\"><img decoding=\"async\" width=\"1800\" height=\"598\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution.png\" class=\"img-responsive wp-image-1131\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution-200x66.png 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution-400x133.png 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution-600x199.png 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution-800x266.png 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution-1200x399.png 1200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Tect-evolution.png 1800w\" sizes=\"(max-width: 800px) 100vw, 1800px\" \/><\/a><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:50px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-2\"><p><span style=\"color: #808080;\">(Last update: 20.05.2020)<\/span><\/p>\n<\/div><div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-89","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/89","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/comments?post=89"}],"version-history":[{"count":27,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/89\/revisions"}],"predecessor-version":[{"id":1316,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/89\/revisions\/1316"}],"wp:attachment":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/media?parent=89"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}