{"id":18,"date":"2018-01-26T15:21:59","date_gmt":"2018-01-26T13:21:59","guid":{"rendered":"http:\/\/minsysfin.gtk.fi\/?page_id=18"},"modified":"2020-06-15T14:46:38","modified_gmt":"2020-06-15T11:46:38","slug":"traps-and-footprints","status":"publish","type":"page","link":"https:\/\/minsysfin.gtk.fi\/index.php\/traps-and-footprints\/","title":{"rendered":"Au-only deposits"},"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-clearfix\"><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_2_3 2_3 fusion-two-third fusion-column-last\" style=\"width:66.666666666667%;width:calc(66.666666666667% - ( ( 4% ) * 0.66666666666667 ) );margin-top:0px;margin-bottom:0px;\"><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><b>Examples<\/b><b> of <\/b><b>altered<\/b> <b>lower<\/b> <b>amphibolite<\/b> <b>facies<\/b><b>\u00a0 <\/b><b>q<\/b><b>uartz-feldspar<\/b> <b>prorphyry<\/b> <b>from<\/b><b> the Mataralampi <\/b><b>gold <\/b><b>deposit<\/b><b>, Kuhmo-Suomussalmi <\/b><b>greenstone<\/b> <b>belt<\/b>.<\/p>\n<\/div><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_3 1_3 fusion-one-third fusion-column-first\" style=\"width:33.333333333333%;width:calc(33.333333333333% - ( ( 4% + 4% ) * 0.33333333333333 ) );margin-right: 4%;margin-top:-60px;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-2\"><p>In all Finnish orogenic gold deposits investigated in detail and analysed with an extensive set of elements, we see the following features, independent of regional metamorphic grade, host rock type, or age:<\/p>\n<ul>\n<li>Alteration is characterised by potassic mica, carbonate(s), and minor iron sulphides replacing pre-existing minerals also resulting in CO2, K, Rb, and S enrichment in the system<\/li>\n<li>Deposits and their immediate wall rocks are enriched in Ag, As, Bi, Sb, Te and W (Download Excel table:\u00a0<a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Enriched_by_belt.xlsx\">Enriched by belt)<\/a>; there are very few exceptions where one of the listed potential pathfinders is not enriched in an occurrence, in any greenstone or schist belt, or a deposit camp<\/li>\n<li>Mobility of Al, Ca, Fe, Mg, Mn, Ti, Zr has not been detected<\/li>\n<\/ul>\n<p>Depending on regional metamorphic grade, the following mineral assemblages characterise proximal alteration:<\/p>\n<p>Download Excel table: <a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Oreminerals_alteration_by-belt.xlsx\">Oreminerals<\/a><a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Oreminerals_alteration_by-belt.xlsx\"> alteration by belt<\/a><\/p>\n<p>Download Excel table: <a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Orogenic_alteration_sequences.xlsx\">Orogenic<\/a><a href=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/Orogenic_alteration_sequences.xlsx\"> alteration sequences<\/a><\/p>\n<\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:5px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-3\"><p>Alteration mineralogy according to the metamorphic grade of the host rock:<\/p>\n<ul>\n<li>Lower- and mid-greenschist facies: muscovite\u2013ferrous dolomite (or ankerite)\u2013albite\u2013quartz\u2013rutile\u2013pyrite \u00b1 arsenopyrite<\/li>\n<li>Upper-greenschist facies: biotite or muscovite\u2013ferrous dolomite (or ankerite)\u2013albite\u2013rutile\u2013pyrite \u00b1 arsenopyrite, pyrrhotite<\/li>\n<li>Lower-amphibolite facies: biotite\u2013calcite\u2013calcic amphibole\u2013plagioclase\u2013ilmenite\u2013pyrrhotite \u00b1 pyrite, arsenopyrite, l\u00f6llingite<\/li>\n<li>Mid-amphibolite facies and higher PT: biotite\u2013calcite\u2013clinopyroxene\u2013calcic amphibole\u2013plagioclase\u2013ilmenite\u2013pyrrhotite \u00b1 l\u00f6llingite, arsenopyrite<\/li>\n<li>In ultramafic rocks, fuchsite or phlogopite instead of muscovite or biotite, respectively<\/li>\n<li>In felsic to intermediate rocks, muscovite may occur in addition to biotite also in amphibolite-facies terrain<\/li>\n<\/ul>\n<p>There is no relationship between the presence of As-rich sulphides and metamorphic grade. Just the presence of l\u00f6llingite, in addition to arsenopyrite, requires amphibolite-facies conditions.<\/p>\n<p>Alteration and the disseminated sulphides in amphibolite-facies hosted deposits can be difficult to see. The main alteration product is biotite which also is common in unaltered assemblages and, especially in granitoid-hosted deposits, the grain size of sulphides tends to be very small. In such cases, the most obvious indication of mineralisation in outcrop are the rusty quartz veins with rusty, foliated envelopes.<\/p>\n<\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-4\"><p><strong>Other examples:<\/strong><\/p>\n<p><a href=\"https:\/\/minsysfin.gtk.fi\/index.php\/pampalo\/\" aria-current=\"page\">&gt; Pampalo, Archaean Hattu schist belt<\/a><\/p>\n<p><a href=\"https:\/\/minsysfin.gtk.fi\/index.php\/suurikuusikko\/\">&gt; Suurikuusikko, Paleoproterozoic Central Lapland greenstone belt<\/a><\/p>\n<\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-5\"><p><span style=\"color: #808080;\">(Last update: 20.05.2020)<\/span><\/p>\n<\/div><div class=\"fusion-clearfix\"><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-3 fusion_builder_column_1_3 1_3 fusion-one-third\" style=\"width:33.333333333333%;width:calc(33.333333333333% - ( ( 4% + 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;\"><span class=\" fusion-imageframe imageframe-none imageframe-1 hover-type-none\"><img decoding=\"async\" width=\"796\" height=\"688\" alt=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 1\" title=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 1\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_1.jpg\" class=\"img-responsive wp-image-330\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_1-200x173.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_1-400x346.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_1-600x519.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_1.jpg 796w\" sizes=\"(max-width: 800px) 100vw, 600px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-6\"><p>Least altered. All phenocrysts well preserved. Mineral assemblage quartz-albite-K feldspar-biotite-titanite \u00b1 muscovite, calcite, rutile. Sample length 11 cm. Photo Reijo Lampela, GTK.<\/p>\n<\/div><span class=\" fusion-imageframe imageframe-none imageframe-2 hover-type-none\"><img decoding=\"async\" width=\"887\" height=\"530\" alt=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 3\" title=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 3\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3.jpg\" class=\"img-responsive wp-image-332\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3-200x120.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3-400x239.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3-600x359.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3-800x478.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_3.jpg 887w\" sizes=\"(max-width: 800px) 100vw, 600px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-7\"><p>Proximal alteration with intense shearing. Mineral assemblage: muscovite-quartz-albite-calcite-rutile-pyrite \u00b1 K feldspar(?). Sample length 7.5 cm. Photo Reijo Lampela, GTK<\/p>\n<\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:32px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-8\"><p><b>O<\/b><b>rogenic<\/b><b> gold <\/b><b>deposit<\/b><b> in <\/b><b>amphibolite<\/b> <b>facies<\/b> <b>rocks<\/b><b>, <\/b><b>Kaapelinkulma, Pirkanmaa <\/b><b>belt<\/b><\/p>\n<\/div><span class=\" fusion-imageframe imageframe-none imageframe-3 hover-type-none\"><img decoding=\"async\" width=\"768\" height=\"1024\" alt=\"Kaapelinkulma, Pirkanmaa belt\" title=\"Kaapelinkulma, Pirkanmaa belt\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-768x1024.jpg\" class=\"img-responsive wp-image-325\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-200x267.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-400x534.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-600x800.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-800x1067.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt-1200x1601.jpg 1200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/kaapelinkulma_pirkanmaa_belt.jpg 1473w\" sizes=\"(max-width: 800px) 100vw, 600px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-9\"><p>Gold-mineralised shear zone in quartz diorite. Photo Pasi Eilu.<\/p>\n<\/div><div class=\"fusion-clearfix\"><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-4 fusion_builder_column_1_3 1_3 fusion-one-third fusion-column-last\" style=\"width:33.333333333333%;width:calc(33.333333333333% - ( ( 4% + 4% ) * 0.33333333333333 ) );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;\"><span class=\" fusion-imageframe imageframe-none imageframe-4 hover-type-none\"><img decoding=\"async\" width=\"859\" height=\"539\" alt=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 2\" title=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 2\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2.jpg\" class=\"img-responsive wp-image-331\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2-200x125.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2-400x251.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2-600x376.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2-800x502.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_2.jpg 859w\" sizes=\"(max-width: 800px) 100vw, 600px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-10\"><p>Intermediate alteration. Quartz phenocrysts distinct, feldspar phenocrysts less easy to detect. Mineral assemblage quartz-albite-K feldspar-biotite-muscovite-calcite-rutile. Sample length 9.5 cm. Photo Reijo Lampela, GTK.<\/p>\n<\/div><span class=\" fusion-imageframe imageframe-none imageframe-5 hover-type-none\"><img decoding=\"async\" width=\"861\" height=\"749\" alt=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 4\" title=\"Mataralampi Kuhmo Suomussalmi greenstone belt, Fig. 4\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4.jpg\" class=\"img-responsive wp-image-333\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4-200x174.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4-400x348.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4-600x522.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4-800x696.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/mataralampi_kuhmo_suomussalmi_greenstone_belt_4.jpg 861w\" sizes=\"(max-width: 800px) 100vw, 600px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-11\"><p>Proximal alteration with intense shearing, sericization and carbonatization. Mineral assemblage: muscovite-quartz-albite-calcite-rutile-pyrite \u00b1 K feldspar(?). Sample length 5 cm. Photo Reijo Lampela, GTK.<\/p>\n<\/div><div class=\"fusion-text fusion-text-12\"><p><b>O<\/b><b>rogenic<\/b><b> gold <\/b><b>deposit<\/b><b> in <\/b><b>amphibolite<\/b> <b>facies<\/b> <b>rocks<\/b><b>, <\/b><b>Arpola<\/b> <b>lode<\/b><b>, Jokisivu <\/b><b>mine<\/b><b>, H\u00e4me <\/b><b>belt<\/b><\/p>\n<\/div><span class=\" fusion-imageframe imageframe-none imageframe-6 hover-type-none\"><img decoding=\"async\" width=\"773\" height=\"1030\" alt=\"Arpola lode, Jokisivu mine, Hame belt\" title=\"Arpola lode, Jokisivu mine, Hame belt\" src=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541-773x1030.jpg\" class=\"img-responsive wp-image-321\" srcset=\"https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541-200x267.jpg 200w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541-400x533.jpg 400w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541-600x800.jpg 600w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541-800x1067.jpg 800w, https:\/\/minsysfin.gtk.fi\/wp-content\/uploads\/arpola_lode_jokisivu_mine_hame_belt-e1569502794541.jpg 1104w\" sizes=\"(max-width: 800px) 100vw, 773px\" \/><\/span><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-text fusion-text-13\"><p>Auriferous quartz veins, sulphidation (rusty domains) in diorite. Compass plate is 11 cm long. Photo Pasi Eilu.<\/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-18","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/18","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=18"}],"version-history":[{"count":54,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/18\/revisions"}],"predecessor-version":[{"id":1315,"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/pages\/18\/revisions\/1315"}],"wp:attachment":[{"href":"https:\/\/minsysfin.gtk.fi\/index.php\/wp-json\/wp\/v2\/media?parent=18"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}