Metallogeny of Eocene Syncollisional Granites of Motajica and Prosara Mountains
نویسنده
چکیده
The geological setting is dominated by Eocene (48.7 Ma) syncollisional granitoids in the form of a small pluton in the Motajica Mt. and in the form of numerous sills and dykes in the Prosara Mt. Microelement paragenesis of these magmatites, pegmatites, greisens and quartz veins are distinguished by U, Th, Ce, Y, P, Nb, Ta, B, Li, F, Be, Sn, Mo, W, Fe, Cu, Pb. These elements and 87Sr/86Sr and δ18O isotopic values indicate the mantle origin of magma contaminated by relatively sterile lithospheric rocks. The most probable hypothesis of such a hybrid magma formation is the “slab break-off model”. Deep erosion of Motajica granitoid pluton opened its acrobatholitic and epibatholitic level with numerous, but small pegmatite deposits (beryllites, tourmalinites, emeraldites and sylexites with piezoelectric quartz). Greisenization marked by strong silicification and muscovitization affected less than 1% of pluton. It is characterized by minor and accessory molybdenite, wolframite, huebnerite, scheelite, fluorite. Hydrothermal occurrences, galena and Fe minerals have only a mineralogical significance. Economically significant are numerous autochthonous kaolin deposits formed in Pliocene-Pleistocene time. Prosara apomagmatic granitoids, exclusively granite dykes are metallogenetically sterile. Ključne riječi: Planine Motajica i Prosara, sjeverna Bosna. Eocenski sinkolizioni granitoidi. pegmatiti, grajzeni, kvarcne žile, kaolin. Sažetak Eocenski (48.7 Ma) sinkolizioni granitoidi izgrađuju Motajicu u obliku malog plutona te kao brojni silovi i dajkovi Prosaru. Parageneze mikroelemenata tih magmatita, pegmatita, grajzena i kvarcnih žila: U, Th, Ce, Y, P, Nb, Ta, B, Li, F, Be, Sn, Mo, W, Fe, Cu, Pb kao i vrijednosti 87Sr/86Sr te δ18O indiciraju porijeklo magme iz omotača koja ja kontaminirana relativno metalogeno sterilnim stijenama litosfere. Najvjerojatnija hipoteza formiranja takove hibridne magme je “slab break-off model”. Duboka erozija granitoidnog plutona Motajice otvorila je njegov akroi epibatolitski nivo sa brojnim skromnim ležištima pegmatita (beriliti, turmaliniti, esmerladiti, sileksiti, s piezoelektričnim kvarcem). Grajzenizacijom je zahvaćeno manje od 1 % plutona i karakterizira je izrazita silifikacija i muskovitizacija granitoida sa sporednim ili akcesornim molibdenitom, volframitom, hibneritom, šelitom, fluoritom. Hidrotermalne pojave galenita i Fe minerala imaju samo mineraloški značaj. Značajna su u ekonomskom smislu autohtona ležišta kaolina formirana na granitoidima u pliocen-pleistocenu. Apomagmatske granitoidne, isključivo žilne stijene planine Prosare su metalogenetski sterilne.
منابع مشابه
IGCP Project 510 “A-type Granites and Related Rocks through Time”: Project vita, results, and contribution to granite research
The IGCP 510 project Global Correlation of A-type Granites and Related Rocks, their Mineralization, and Significance in Lithospheric Evolution (or, in short, A-type Granites and Related Rocks through Time) of the International Geoscience Programmewas developed in the period of 2005 to 2010 with the sponsorship of the International Union of Geological Sciences (IUGS) and United Nations Education...
متن کاملسنگشناسی و ژئوشیمی گرانیتوئیدهای سیاه منصور شمالشرق میانه (شمالغرب ایران)
The Siyahmansour area is located between longitude 370 46َ 07" to 370 50َ 19" N and latitude 470 53ً 13" to 470 58َ 22" E in northeastern town of Miyaneh Exposure of different igneous rocks in the studied area including Eocene to Miocene volcanic rocks, granitoids and diorites. The granitoids are different including muscovite granites and granite-granodiorite. The muscovite granites are intruded in...
متن کاملGeochemical evolution and petrogenesis of the eocene Kashmar granitoid rocks, NE Iran: implications for fractional crystallization and crustal contamination processes
Kashmar granitoids of Taknar zone, in north part of Lut block, intruded into volcanic rocks and consist of granites, granodiorites, monzodiorite and gabbrodiorites. They are composed of mainly plagioclase, alkali-feldspar, quartz, amphibole, biotite and pyroxene minerals. Harker diagram variation, including negative correlations CaO, MgO, FeO, TiO2 and V and positive correlations K2O, Rb, Ba, a...
متن کاملبررسی خاستگاه و زمین دما-فشارسنجی تودههای گرانودیوریتی و گرانیتی شاهجهان: با کاربرد دادههای ایزوتوپ ناپایدار، سنسنجی و ژئوشیمی
The Shah Jahan Granodiorite and granite rocks are part of the Ordubad granitoid body that outcrop in 10 km south of Aras River. These rocks are located in the Alborz-Azerbaijan zone in NW of Iran. The Granodiorite Pluton has granular texture; containing minerals are plagioclase (andesine), alkali feldspar (orthoclase), amphibole (magnesio-hornblende) biotite, titanite and magnetite. Alkali feld...
متن کاملDetermination of the Geological Conditions During the Formation of Kaolinite and Bentonite Deposits in NW Alborz Mountains (Pirkoh-Deylaman) of Iran and the Study of Its Practical Properties for Use in the Porcelain Industry
The area under study is located in northern Iran at 36° 47’ latitude and 50° 12' longitude. It is 15 km from southeastern Deylaman. Petrological study of the kaolin mother rock (Eocene age) under a microscope shows that the rock is vitric tuff with a rhyolitic combination containing falcated and embowed glass shards. The thickness of the layer is approximately 20 meters, formed unconformably on...
متن کامل