Hoạt động magma liên quan đến điểm nóng lục địaCác tỉnh thạch học lớn Large Igneous Provinces - LIPs Kimberlit và lamprroit Columbia River Basalts at Hat Point, Snake River area.. Hoạt đ
Trang 1Hoạt động magma liên quan đến điểm nóng lục địa
Các tỉnh thạch học lớn (Large Igneous Provinces - LIPs)
Kimberlit và lamprroit
Columbia River Basalts at Hat Point, Snake River area
Cover of Geol Soc Amer Special Paper 239 Photo courtesy Steve Reidel.
Trang 21 – Yakutian, 2 – Arkhangelsk, 3 – East China, 4 – North Australia, 5 – South Africa,
6 – Central Africa, 7 – West Africa, 8- Brazil, 9 – Venezuela GRB –Rio Grande
basalts, NATB – North-Atlantic Tertiary basalts (modified from Pirajno, 2003)
Parana
GRB
Yellowstone Wrangellina
Tristan Louisville
Iceland
NATB
Siberian
Balleny Kergulen
Hess
Marion
8910
567
12
Trang 3Hoạt động magma rift lục địa (rift cổ và trẻ) Basalt lũ (phủ tràn lục địa - trap)
Kimberlit và lamprroit
Trang 4Figure 15-2 Flood basalt provinces of Gondwanaland prior to break-up and separation After Cox (1978) Nature, 274, 47-49
Trang 5Figure 15-3 Relationship of the Etendeka and Paraná plateau provinces to the Tristan hot spot After Wilson (1989), Igneous Petrogenesis Kluwer.
Trang 6CÁC TỔ HỢP MAGMA CỦA RIFT LỤC ĐỊA
Loạt phonolit và bazanit
Bazan kiềm – trachyt
Bazan - riolit
Trang 7CÁC TỔ HỢP MAGMA KIỂU TRAP
Trang 8Geologic map of the NW Siberian Platform showing distribution of Paleozoic
sediments and Siberian flood-volcanic rocks in the Maymecha-Kotuy and Noril’sk areas East of these areas are Proterozoic sedimentary rocks and Archean gneisses of
the Anabar Shield In quadrangles are sample locations for zircon dating
J-K sidementaryrocks
Ptz sedimentaryrocks1
Studied samples ofvolcanic rocksStudied samples ofthe Noril’sk intrusion
Studied sample ofthe Bolgakhtokh intrusion
the first stage P-T volcanic rocks
21
Ar-Ptz gneisses ofthe Anabar Shield
1
Є-P sidementaryrocks
Trang 9Legend
TrapsBasalts, dike complexes of basites & alkaline basites
Deposits
Cu-Ni-Pt Ni-Co-As
Hg and Au-Hg Cu-Mo porphyry
Trang 10Figure 15-6 Variation in wt.% of selected major element oxides vs Mg# for units of the Columbia River Basalt Group Winter (2001) An Introduction
to Igneous and Metamorphic Petrology Prentice Hall Data from BVTP (Table 1.2.3.3), Hooper (1988a), Hooper and Hawkesworth (1993)
Trang 11Figure 15-7 Condrite-normalized rare earth element patterns of some typical CRBG samples Winter (2001)
An Introduction to Igneous and Metamorphic Petrology Prentice Hall Data from Hooper and Hawkesworth
(1993) J Petrol., 34, 1203-1246
Trang 12Figure 15-8 N-MORB-normalized spider diagram for some representative analyses from the CRBG Winter (2001) An
Introduction to Igneous and Metamorphic Petrology Prentice Hall Data from Hooper and Hawkesworth (1993) J Petrol.,
34, 1203-1246 Picture Gorge from Bailey (1989) Geol Soc Amer Special Paper, 239, 67-84
Trang 13Figure 15-9 OIB-normalized spider diagram for some representative CRBG analyses Winter (2001) An Introduction to Igneous and Metamorphic Petrology Prentice Hall (data as in Figure 15-8)
Trang 14Figure 15-11 87 Sr/ 86 Sr vs 143 Nd/ 144 Nd for the CRBG Winter (2001) An Introduction to Igneous and Metamorphic
Petrology Prentice Hall Data from Hooper (1988a), Carlson et al (1981), Carlson (1984), McDougall (1976), Brandon et al (1993), Hooper and Hawkesworth (1993)
Trang 15Figure 15-11 208 Pb/ 204 Pb vs 206 Pb/ 204 Pb for the basalts of the CRBG Included for reference are EMI, EMII, the DUPAL group, the MORB array, and the NRHL (northern hemisphere reference line) connecting DM and HIMU mantle reservoirs from Figure 14-6 Winter (2001) An Introduction to Igneous and Metamorphic Petrology
Prentice Hall Data from Hooper (1988a), Carlson et al (1981), Carlson (1984), McDougall (1976), Brandon et al
(1993), Hooper and Hawkesworth (1993)
Trang 16Figure 15-14 Diagrammatic cross section illustrating possible models for the development of continental flood basalts DM is the depleted mantle (MORB source reservoir), and the area below 660 km depth is the less depleted, or enriched OIB source reservoir Winter (20010 An Introduction to Igneous and Metamorphic Petrology Prentice Hall.
Trang 19Isotope ages of Song Da komatiite
Trang 20Distribution of REE in basalt association of Song Da rift, Emeishan and Siberian traps, normalized to chondrit
komatiite-(Sun&M.Donough, 1989)
Spider-diagramm for
komatiite-basalt association of Song Da rift,
Emeishan and Siberian traps,
normalized to PM (Sun
&M.Donough, 1989)
Trang 21Spider-diagramm of NW Song Da High-Ti basalts in comparision with Emeishan’s
Spider-diagramm of SE Song Da
High-Ti basalts in comparision
with Emeishan’s
Trang 22KIMBERLIT VÀ LAMPROIT
VỊ TRÍ KIẾN TẠO:
Kimberlit thường ở trong craton (trong nền);
Lamproit thường đặc trưng cho các đai động ven nền.