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Section 7, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It discusses the evolution of the Central Lapland greenstone belt associated with plume-related, intracratonic rift magmatism. It discusses the deposition of Lainio and Kumpu group arenitic and rudaceous sediments into the foreland basin.

Section 6, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It discusses the formation of metavolcanic rocks relative to the incipient mantle plume in the initial stages of continental rifting. It provides an overview on the geochemical and isotopic features volcanic rocks found mainly as subaerially erupted lavas.

Section 4, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It describes the layered mafic intrusions in the Akanvaara and Koitelainen shields, located within the Central Lapland greenstone belt. It offers information on the level of chromitite reserves in these shields.

Section 3, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the general characteristics of the Central Lapland greenstone belt. It also discusses the increase of regional metamorphism towards the granitoid complex in the south and Svecofennian granites in the west.

Section 6, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the geological, structural and geochemical characteristics of the Tornio-Näränkävaara belt. It discusses the location of layered intrusions that were formed in a mantle-related intracratonic breakup of the Archean craton.

Section 5, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the different types of ore deposits discovered in theTornio-Näränkävaara intrusion belt. An overview on the classification of three main types of these deposits is provided.

Section 3, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O.T. Rämö is presented. It describes the general characteristics of the stratigraphy of the Tornio-Näränkävaara belt. Information on the layered marginal series on the different intrusions in the western and central parts of the belt is provided.

Section 5, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the geographic borders and description of the terranes of granulite belt in Central Lapland. It discusses the three main types of granulites within this belt.

Section 1, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the evolution of the greenstone belt in Central Lapland. It discusses the formation of supracrustal rock sequence through deposition.

Section 4, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O.T. Rämö is presented. It describes the characteristics of the parental magma of the layered intrusions in the Tornio-Näränkävaara belt. An overview on the weighted chemical compositions of representative rock samples is provided.

Section 2, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the geologic setting of the Tornio-Näränkävaara belt, a discontinuous zone of layered intrusions crossing the country, Arctic Circle and Russia. It provides an overview on the different types of minerals present in this belt.

Section 1, Chapter 3 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the layered mafic-ultramafic intrusions found in the Tornio-Näränkävaara belt. It provides an overview on the different types of minerals present in these intrusions.

Section 2, Chapter 4 of the book "Precambrian Geology of Finland: Key to the Evolution of the Fennoscandian Shield," edited by M. Lehtinen, P. A. Nurmi and O. T. Rämö is presented. It offers information on the main layered mafic-ultramatic intrusion units in the Central Lapland greenstone belt located in the northern part of the country. It provides an overview on the different rock minerals found in this belt.