Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa)...

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Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components to Define Mantle Composition? Armienti and Gasperini - J. Petrology 48: 693 and Three-dimensional representation of geochemical data from a multidimensional compositional space. Armienti and Longo - Int, Jour. of Geosciences. In press

Transcript of Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa)...

Page 1: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Projections and trickstools to test petrogenetic ipotheses

Pietro Armienti (Università di Pisa)

based on the papersDo We Really Need Mantle Components to Define Mantle Composition?

Armienti and Gasperini - J. Petrology 48: 693 and

Three-dimensional representation of geochemical data from a multidimensional compositional space.

Armienti and Longo - Int, Jour. of Geosciences. In press

Page 2: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

This analysis of data is based on an algorithm

which projects data from a multi-dimensional space in

three-dimension

Page 3: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

y

x

AB

E

E*

B A E* = B + 1 v

1 v1

v1 = A - B

The projection scheme from Rn to R3 may be envisaged by looking at the analogue for the projection from a plane onto a segment AB.

In a 2D space two points B, A

visualize the 1D space onto which to map E (x, y)

onto E* ().

Page 4: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

In a similar way four points “materialize” the 3D space onto which to project data from Rn

EM I

HIMU

EM II

DMM

EMI-EMII

OIB-EMII

DMM-EM1

OIB-EM1

OIB-DMM

DMM-EMII

linea

Canary

Hawaii

St. Helena

SAmoa

Canary

Azzorre

Australi

EM I

HIMU

EM II

DMM

EMI-EMII

OIB-EMII

DMM-EM1

OIB-EM1

OIB-DMM

DMM-EMII

linea

St. Helena

SAmoa

Azzorre

Australi

For simplicity’s sake, the four points (“end-members”) are mapped onto the vertices of a regular tetrahedron

Page 5: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitiveSp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitiveSp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitiveSp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive SpCpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive SpCpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive SpCpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive SpCpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitiveSp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

Sp

Cpx

OVP18 106

Ol

linea

ovp

BRP

BR

WR

Da FusioneAmphKaersutite

pargasite

Clinopirosseni

Ortopirosseni

Olivina

Spinello

EMI-EMII

OIB-DMM

DMM-EMII

OIB-EM1

OIB-EMII

DMM-EM1

Lave primitive

By choosing a suitable set of four end-

members, each defined by its components (e.g.

minerals and major elements), the

tetrahedron vertices attract the projection of the given analyses. The

method allows to project points with negative

values of the end-members to obey mass

balance constraints

Page 6: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

(b)Di

(d)Q

(c)Ol

(a)S

Sp

Ol

Di

CaTs

active values C M A Sselect

projectiona CaTs 18,693 ,000 33,987 20,030 0

b Di 14,020 10,008 ,000 30,045 1

c OL ,000 26,687 ,000 20,030 0

d Q ,000 ,000 ,000 60,090 0y/n 1,0 1,0 1,0 1,0 none

(b)Di

(d)Q

(a)S

(c)Ol

Sp

CaTs

Di

Ol

… allowing also to project data onto a face of the tetrahedron from the opposite vertex.

The same scheme allows also to project relevant phase relations in petrologic diagrams

Page 7: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

In systems with many components, compositions are often re-calculated in terms of end members, like in normative calculations that allow to recast the analysis of a rock in terms of fictive anhydrous minerals.

Ne

Ol

Di

En

Ab

SiO2 TiO2 Al2O3 Fe2O3 FeO MnO MgO CaO Na2O K2O p2O5

p.M. 60,0855 79,88 101,96 159,694 71,847 70,938 40,305 56,08 61,9795 94,1966 141,95

Analisi wt% 47,72 1,71 17,91 2,42 7,61 0,00 5,60 9,95 3,80 1,84 0,45

47,72 1,71 17,91 2,42 7,61 0,00 5,60 9,95 3,80 1,84 0,45

47,72 1,71 17,91 2,42 7,61 0,00 5,60 9,95 3,80 1,84 0,45

Page 8: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

B

D

A

C

X

Y

Z

r

r

O

E F

"canonical" orientation of the tetrahedron whose centre is in the origin of the axes and the XA,YA,ZA coordinates of vertex A are (0,0,r) while the edge CB forms an angle f with the Y axis (It follows for the XB,YB, ZB coordinates of B

13) XB = r*sin ()*sin() 14) YB = r*sin ()*cos()15) ZB = r*cos()

being the angle AOB ;

Page 9: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

B

D

A

C

X

Y

Z

r

r

O

E F

coordinates of vertices C e D are obtained substituting with (+120) and (+240) respectively. Varying causes the tetrahedron to rotate around Z.

Rotating around the X axis of an angle , the new coordinates

Xi', Yi', Zi' are related to the old ones by the equations :

16) Xi’ = Xi*cos()+z*cos()17) Yi’ = Yi18) Zi’ = -Xi*sin()+Zi*cos()

Page 10: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

To plot a point P(Ap,Bp,Cp,Dp) within the tetrahedron and get P(Xp,Yp,Zp) we can start projecting E on the edge AB on the basis of the ratio Bp/Ap, calculating the coordinates of this point P'(Xp’,Yp’,Zp’);19a) Xp ’= (XA + Bp/Ap * XB)/(1+ Bp/Ap)19b) Yp’ = (YA + Bp/Ap * YB)/(1+ Bp/Ap)19c) Zp’ = (ZA + Bp/Ap * ZB)/(1+ Bp/Ap)

A

B C

D

P’

Page 11: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

then P is projected onto the face ABC, as a function of the Cp/(Ap+Bp) and the coordinates of this point P”(X p”, Y p”, Z p”);

20a) Xp” = (Xp’+ (Cp/(Ap+Bp)* Xc)/(1+ Cp/(Ap+Bp)) 20b) Yp” = (Yp’+ (Cp/(Ap+Bp)* Yc)/(1+ Cp/(Ap+Bp))20c) Zp” = (Yp’+ (Cp/(Ap+Bp)* Zc)/(1+ Cp/(Ap+Bp))

A

B C

D

P’

P’’

Page 12: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

At last, the coordinates of P within the tetrahedron are found on the segment P”D tracing on P”D a segment P”P as required by the lever rule : P”P/DP= Dp/(Ap+Bp+Cp). 21a) Xp = (Xp” +(Dp/(Ap+Bp+Cp).)*XD)/(1+(Dp/(Ap+Bp+Cp)) 21b) Yp = (Yp” +(Dp/(Ap+Bp+Cp).)*YD)/(1+(Dp/(Ap+Bp+Cp))21c) Zp = (Zp” +(Dp/(Ap+Bp+Cp).)*ZD)/(1+(Dp/(Ap+Bp+Cp))

A

B C

D

P’

P’’P

Page 13: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Let us assume that a system E, whose composition is described in terms of n components (e.g. major elements), can be referred to a set of four end members A,B,C,D and that each of them can be represented in terms of the same set of n components. E, A, B, C and D can be represented as points in n-dimensional space (Rn ).

E(E1, …En)

Considering A, B, C, D as the vertices of a tetrahedron in Rn, we need relations that are able to represent the point E(E1, …En) in n-dimensional space in terms of four end members : A(A1,...,An), B (B1,...,Bn), C (C1,...,Cn), D (D1,...,Dn).

Page 14: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

The algorithm has to assign to E four coordinates (AE,BE,CE,DE) that allow its projection in a 3D tetrahedron that can be easily plotted

B

D

A

C

X

Y

Z

O

E

G

Page 15: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

The algorithm is derived extending in Rn the rules for the projection of a point E(e1, …en) in a R3 tetrahedron: the procedure can be summarized as below:

1. Assign in Rn the coordinates of the tetrahedron vertices: A(a1,...,an),

B(b1,...,bn), C(c1,...,cn), D(d1,...,dn) B

D

A(a1,a2,a3,a4)

C

G

E(e1,e2,e3,e4)

Page 16: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

B

D

A

C

X

Y

Z

O

E

G

+

2 To assign the coordinate AE find in Rn the intersection E' (E'1,...,E'n ) between the line through AE and the hyperplane through BCD,

3 Compute the lengths of segments AE', EE' and AE

E’

Page 17: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

4. following the lever rule, assign to AE the value : 100-100*(AE’-EE’)/AE’= 100*EE'/AE'.

Repeat the steps from 2 to 4 to compute BE,CE,DE changing the vertex and the plane onto which to project E.

B

D

A

C

X

Y

Z

O

E

G

+

Page 18: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Computing tetrahedral coordinates in this way ensures that for all the points falling inside the tetrahedron AE + BE + CE + DE = 100,

B

D

A

C

X

Y

Z

r

r

O

E

FG

E

E

E’

Page 19: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

This sum is different from 100 for points that in Rn lay outside the tetrahedron.

B

D

A

C

X

Y

Z

r

r

O

E

FG

E

E

E’

To allow the representation of these points in R3 we have to allow for negative tetrahedral coordinates: this is easily accomplished by comparison of lengths of segments AE, EE’ and AE’, it is easy to realize that:

Page 20: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

•For points that are inside the tetrahedron AE’=AE+EE’.

•For points that are below the face BCD, EE’ may be smaller or larger than AE’, but AE<AE’ and EE’ is to be taken in equation 12 with a negative sign.

•For points that are above vertex A, EE’ > AE’ and EE’ has to be taken in equation 12 with a positive sign,

B

D

A

C

X

Y

Z

r

r

O

E

FG

E

E

E’

Page 21: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

To obtain the 3D projection E* of E:

1)  assign tetrahedron vertices (end members) A,B,C,D Rn , and compute vectors

v1 =A-D, v2 = B-D, v3 =C-D

Set and ;

w1= v1 and

Lastly, set and

2 α

||v||

vv

1

12 2

3 ||v||

vv

1

1

122 wvw α

22

23 ||w||

wv 233 wwvw 1

Page 22: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

2) For each point to project

compute the vector E’=E- D

and its orthogonal projection E” on <w1,w2,w3 > ,

that is E” = 1w1+2w2+3w3

where i = , i = 1, 2 , 3.

E” is the linear combination of w1,w2,w3 nearest to E’ in Rn. Since the distance is translation-invariant, it follows that

E*=D+1v1+2v2+3v3 is the point in the 3D-space passing through A,B,C,D nearest to D + E’=E .

•  

2||w||

wE

i

i'

Page 23: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

3) Finally, remark that

E*= D +1w1+2w2+3w3

= D+1(A–D)+2[ B–D - (A–D)] +

+3{ C–D-(A–D) -[ B–D- (A–D)]}=

=(1-2-3+3 A (2-3 B 3 C+

+ (1-2-3+2+3+3 -3 D

The sum of the four coefficients of the end members at the right hand of the above formula, is 1; therefore, they represent the tetrahedral coordinates i of E* with respect to the four vertices A,B,C,D:

Page 24: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Tetrahedral coordinates1= 1-2-3+3

2= 2-3

3= 3

4 = 1-2-3+2+3+3 -3 1 - 2 -

3The point E* coincides with E if and only if E itself is a linear combination in Rn of the end members with sum of coefficients equal to one. Otherwise, E* is distinct from E, while enjoying the property to be at the minimal Euclidean distance from it, among all points of the (affine) subspace passing through the end members.

Page 25: Projections and tricks tools to test petrogenetic ipotheses Pietro Armienti (Università di Pisa) based on the papers Do We Really Need Mantle Components.

Let now (T1,T2,T3,T4) be the vectors in R3 to which the tetrahedron vertices A,B,C,D are mapped on ;

Finally, E will be mapped in R3 onto E* by the relation

E*= 1 T1+2 T2+3 T3+4 T4.

For a regular tetrahedron a possible choice is :

T1=(0,0,1),

T2=(2*2/3,0,-1/3);

T3=(-2/3, 2/3, -1/3);

T4=(-2/3, -2/3, -1/3).